Martin Van Kranendonk

Public profile

Prof Martin Van Kranendonk
Director ACA
+61(2) 9385 2439
Postal Address: 
School of Biological and Earth and Environmental Sciences University of NSW Kensington, 2033 New South Wales, Australia
+61(2) 9385 1558
Grouping Type: 

My research interest is the early Earth, how it formed, how crust developed on the surface and changed over time, and how life gained a foothold on our developing planet. Specifically, I am interested in how the changing Earth system co-evolved with the biosphere through time. My main field-based research in the Pilbara region of Western Australia.

I am a Professor of Geology, with 28 years of mapping and research experience in a variety of structurally complex Precambrian terrains. My main interest is on the early history of the Earth and I have developed an international reputation for my work on Archean tectonics and the geological settings of early life on Earth. More recently, as Chair of the Precambrian Subcommission of the International Commission on Stratigraphy, I have commenced a wholescale review of Precambrian stratigraphy with the aim of revising the Precambrian timescale. My particular skills are mapping and the ability to integrate a wide range of geological data into 4-D models, from the craton to micrometre scale.

            My research on early life has established a connection between the earliest putative fossil remains and low-temperature hydrothermal systems, and recognised that life in the early Archean was already diverse, occupying different niches. Through mapping and collaborative laboratory research, I have developed new and comprehensive geological models for the environments of Earth’s oldest fossils. This research has also helped to establish the biogenicity of ancient fossils, through a wide variety of tests based on field and laboratory studies in collaboration with experts from around the globe. The results have been widely published in major journals and have been used to refine models for the search for life on Mars.

            My research in the Pilbara and Yilgarn cratons of Western Australia has placed me at the forefront of Archean tectonic studies, culminating with the recent publication of a book on “Earth’s Oldest Rocks” (Elsevier, 2007). I have also been guest editor for two special volumes of Precambrian Research (2004), and have authored more than 60 publications in international journals. Specifically, I have helped develop a comprehensive tectonic model for the Archean Pilbara craton over 800 Ma of crustal evolution, and recognised a fundamental change in tectonic processes on earth at c. 3.2 Ga, from vertical-dominated to horizontal-dominated tectonics, including modern-style plate tectonics.

            I am also the Assistant Director of the Australian Centre for Astrobiology, co-leader of IGCP-SIDA Project 599 “The Changing Early Earth”, and Core Member of the International Precambrian Research Centre of China. I am on the editorial boards of Precambrian Research, Geology, Astrobiology, and Episodes.

            I have presented numerous talks at a variety of international specialist and general meetings, both as an invited and keynote speaker, most recently at the European Union of Geosciences meeting in Vienna, and at Goldschmidt2011 in Prague. In 2005, together with Prof. Malcolm Walter (Director, Australian Centre for Astrobiology), I co-organised a field and laboratory workshop on early life on Earth for the international astrobiology community, which was filmed to make a NASA public education outreach program that is available for schools in the USA, UK, Australia, and is online and presented in musea. I have led numerous fieldtrips through the Pilbara Craton for a variety of groups, including the 34th IGC in 2012, 5th International Archean Symposium 2010, and Goldschmidt 2006.

            I have contributed to public outreach through public lectures and contributions to several television documentaries on early Earth, including programs for National Geographic Channel (“Birth of the Earth” in 2005; “Was Darwin Wrong?” in 2006), the BBC (“Atmosphere”, 2008), History Channel (“How life began” in 2007), Discovery Channel (“Making of Continents” in 2006; “Inside Planet Earth” in 2008), and Spanish television.




1) Climate and biological change across the Archean-Proterozoic boundary, 2.5-2.2 Ga

Perhaps the most complete and best exposed geological section across the transition from early, reducing Earth conditions (>2.5 Ga) to more modern, oxidized and cooler Earth (2.2 Ga) – known as the Great Oxidation event, or GOE – is exposed in the southern Pilbara region of Western Australia as the Turee Creek Group. Research on this section to date has uncovered a spectacular section across the GOE transition, from Archean banded iron-formation to Paleoproterozoic glacial diamictites across a transitional unit of jaspilitic- to grey-laminated chert, with conformable contacts that you can put your fingernail on (Photo 1). We are currently investigating the nature of this transitional unit in detail through geochemical analysis, Fe isotopes, and redox-sensitive elements (Mo and PGE). A more expanded section has also been found in which the transition is manifest as eight cherts interbedded with iron-formations that grade to shale.

The rest of the Turee Creek Group is also under detailed investigation, particularly in regards to its sedimentology and geochemistry. Preliminary results clearly indicate at least two, and possibly three, glacial cycles, where previously only one had been recorded (Photo 2). Facies analysis indicates that each of the cycles are associated with sealevel drawdown, which can be used to infer that they were global in scope and that major climate change was associated with the rise of atmospheric oxygen.

In addition, we are investigating biological changes across the GOE. We have discovered a well-preserved assemblage of microfossils permineralized in black chert in deepwater carbonates from the upper part of the Turee Creek Group (Photo 3). These microfossils are morphologically and geochemically distinct from photosynthetic cyanobacterial communities of shallow-water stromatolites. Given the deep water setting and through comparison with modern analogues, we are able to conclude that these represent a sublittoral sulfuretum (sulfur-cycling community) – the first to be recorded in the geological record.

Collaborators: Pascal Philippot (Institute de Physique du Globe de Paris); Clark Johnson (U. Wisconsin-Madison); Ken Williford (Jet Propulsion Laboratory); Kliti Grice and Anais Pages (Curtin University); Malcolm Walter and Rajat Mazumder (UNSW); Bill Schopf (UCLA); Aivo Lepland (Geol. Survey Norway).

MVK Research Project 1


2) Planetary Driver of Environmental Change

The Earth has evolved dramatically over time, from a hot, molten ball (magma ocean) immediately following the giant Moon-forming Impact at c. 4.5 Ga, to the cool planet of today with a dozen or so large tectonic plates that are created at mid-ocean ridges and partly recycled back into the mantle across steep subduction zones. My research on early Earth has suggested that this “modern” (i.e. steep) style of subduction commenced at c. 3.1 Ga, due to a crossover point in time when the amount of conductive heat emanating from the mantle first declined to values beneath the capacity of the crust to lose that heat. This allowed the tectonic plates to grow and to cool and thicken away from mid-oceanic ridges, resulting in the onset of steep subduction (through plate sinking).

Ongoing research into the proposed Mesoarchean change in the tectonic style of the planet includes:

  • Analysis of geochemical proxies of subduction through time, specifically high field strength elements in magmatic rocks, and oxygen and Hf isotopes in zircons. Preliminary results show that onset of steep subduction is accompanied by the start of the supercontinent cycle, which evolved and changed over time, peaking at c. 1 Ga and declining in intensity thereafter (Fig. 1).
  • Analysis of a proposed Paleoarchean suture zone in South Africa, where high-P metamorphic mineral assemblages have been used to infer a suture zone. Detailed mapping in 2012 will be combined with geochronology and geochemistry to test this claim. Preliminary results suggest a more complex situation than previously reported.
  • Analysis of oxygen isotopes in zircons from dated samples from Pilbara, Western Australia. Samples were specifically identified to test the subduction-accretion model developed for this area. Preliminary results show evidence for both high and low oxygen isotope values in zircons dated at exactly the age identified independently for subduction and accretion of the West Pilbara Superterrane, and not from zircons of any other age.

Collaborators: Chris Kirkland (Geol. Survey Western Australia); John Cliff (U. Western Australia)

Figure 1: Schematic diagram of Earth evolution through time, showing steps in crustal growth following on from pulses of mantle heat arising from the aftermath of subduction avalanches during supercontinent amalgamation that were accompanied by changes to Earth tessellation (T1-T4).


3) The North Pole volcanic caldera: habitat of Earth’s oldest stromatolites

The North Pole Dome in the Pilbara Craton, Western Australia, is famous for hosting Earth’s oldest stromatolites within a well-preserved succession of sedimentary and volcanic rocks of the Dresser Formation, Warrawoona Group. Research has indicated a link between life and hydrothermal vents that formed at the tips of growth faults developed within an active volcanic caldera. However, only a small part of the formation has been mapped in detail and it is not known whether life is solely restricted to vent environments or is more broadly spread and possibly even diverse. Ongoing mapping at North Pole will document the life signatures preserved in this unique environment in 4-D and unravel the series of events within the caldera, number of hydrothermal circulation cells andvariations along and across strike in the chemistry of the system.

Figure 2: a) Zoned hydrothermal barite-chert vein: b) Hydrothermal barite curling over stromatolite at vent mouth; c) wrinkly laminated and domical stromatolites; d) diagenetic barite in silicified carbonate; e) hydrothermally-altered pillow basalt (now kaolinite) in caldera footwall. 


Collaborators: Malcolm Walter (UNSW), Franco Pirajno and Marco Fiorentini (University of Western Australia)


Popular articles (3)

Van Kranendonk, M.J. (2018). The setting for the Origin of Life: A geological-geochemical perspective. The Biochemist Magazine “Science in Space” issue, Portland Press Ltd.

Van Kranendonk, M.J., Deamer, D.W., Djokic, T., 2018. Life springs. In: Revolutions in Science, Special edition, Scientific American, July 2018.

Van Kranendonk, M.J., Deamer, D.W., Djokic, T., 2017. Life springs. Scientific American, August 2017, p. 28-35.

Published Books (4)

139) Van Kranendonk, M.J., Bennett, V., Hoffmann, J.E. (2018): Earth’s Oldest Rocks, 2nd edition. Elsevier Inc., Cambridge, MA 02139, United States. 1078 p. ISBN: 978-0-444-63901-1:

138) Roberts, N.M.W., Van Kranendonk, M., Parman, S., Shirey, S., Clift, P.D. (Eds.), 2015. Continent Formation through time. Geological Society, London, Special Publications 389.

137) Van Kranendonk, M.J., Johnston, J. (2009): Discovery trails to Early Earth - A Traveller’s Guide to the east Pilbara region of Western Australia. Geological Survey of Western Australia.

136) Van Kranendonk, M.J., Smithies, R.H., Bennett, V. (Eds.), 2007. Earth’s Oldest Rocks. Developments in Precambrian Geology, Series 15. Elsevier, Amsterdam, 1307pp.

Papers in International Journals and Books (135)

2019 (8)

135) iMOST (International MSR Objectives and Samples Team:  co-chairs: D. W. Beaty, M. M. Grady, H. Y. McSween, E. Sefton-Nash; documentarian: B. L. Carrier; team members: F. Altieri, Y. Amelin, E. Ammannito, M. Anand, L. G. Benning, J. L. Bishop, L. E. Borg, D. Boucher, J. R. Brucato, H. Busemann, K. A. Campbell, A. D. Czaja, V. Debaille, D. J. Des Marais, M. Dixon, B. L. Ehlmann, J. D. Farmer, D. C. Fernandez-Remolar, J. Filiberto, J. Fogarty, D. P. Glavin, Y. S. Goreva, L. J. Hallis, A. D. Harrington, E. M. Hausrath, C. D. K. Herd, B. Horgan, M. Humayun, T. Kleine, J. Kleinhenz, R. Mackelprang, N. Mangold, L. E. Mayhew, J. T. McCoy, F. M. McCubbin, S. M. McLennan, D. E. Moser, F. Moynier, J. F. Mustard, P. B. Niles, G. G. Ori, F. Raulin, P. Rettberg, M. A. Rucker, N. Schmitz, S. P. Schwenzer, M. A. Sephton, R. Shaheen, Z. D. Sharp, D. L. Shuster, S. Siljestrom, C. L. Smith, J. A. Spry, A. Steele, T. D. Swindle, I. L. ten Kate, N. J. Tosca, T. Usui, M. J. Van Kranendonk, M. Wadhwa, B. P. Weiss, S. C. Werner, F. Westall, R. M. Wheeler, J. Zipfel, and M. P. Zorzano) (2019): The Potential Science and Engineering Value of Samples Delivered to Earth by Mars Sample Return, Meteoritics & Planetary Science, vol. 54 (3), p. 667-671 (executive summary only). doi:10.1111/maps.13232; open access web link to full report (Meteoritics & Planetary Science, vol. 54, S3-S152.doi:10.1111/maps.13242.

134) Chilton, A.M., Vázquez-Campos, X., Steller, L.H., Van Kranendonk, M.J. (2019): Microbial profiling of Puga hot springs. Astrobiology, in press.

133) Johnson, C.M., Van Kranendonk, M.J. (2019): Ancient Life and Plate Tectonics (Chapter 4.4). In Kolb, V.M. (ed) Handbook of Astrobiology, pp. 195-205, CRC Press.

132) Nomchong, B., Van Kranendonk, M.J., (accepted): The diversification of life at the rise of atmospheric oxygen: Clotted microbialites from the c. 2.4 Ga Turee Creek Group, Western Australia. Precambrian Research.

131) Nutman, A.P., Friend, C.R.L., Chivas, A., Van Kranendonk, M.J., Bennett, V.C., Rothacker, L. (2019): Cross-examining Earth’s oldest stromatolites: Seeing through the effects of heterogeneous deformation, metamorphism and metasomatism affecting Isua (Greenland) ~3700 Ma sedimentary rocks. Precambrian Research 331, 105347. DOI:10.1016/j.precamres.2019.105347

130) Ruff, S.W., Campbell, K.A., Van Kranendonk, M.J., Rice, M., Farmer, J. (in press): The case for ancient hot springs in Gusev Crater, Mars. Astrobiology.

129) Soares, G., Van Kranendonk, M.J., Belousova, E., Thomson, S. (2019): Phosphogenesis in the immediate aftermath of the Great Oxygenation Event: Evidence from the Turee Creek Group, Western Australia. Precambrian Research 320, 193-212.

128) Steller, L.H., Nakamura, E., Ota, T., Sakaguchi, C., Sharma, M., Van Kranendonk, M.J. (2019): Boron isotopes in the Puga geothermal system, India, and their implications for the habitat of early life. Astrobiology 19, 12. DOI: 10.1089/ast.2018.1966.

2018 (11)

127) Barlow, E.V., Van Kranendonk, M.J. (2018): Snapshot of a c. 2.4 Ga ecosystem: Two diverse microfossil communities from the Turee Creek Group, Western Australia. Geobiology 16(5), 449-475.

126) Cammack, J.N., Picuza, M.J., Cavosie, A.J., Van Kranendonk, M.J., Hickman, A.H., Kozdon, R., Orland, I.J., Kitajima, K., Valley, J.W. (2018): SIMS microanalysis of the Strelley Pool Formation cherts and the implications for the secular-temporal oxygen-isotope trend of cherts. Precambrian Research 304,

125) Czaja, A.D., Van Kranendonk, M.J., Beard, B.L., Johnson, C.M. (2018): A multistage origin for Neoarchean layered hematite-magnetite iron formation from the Weld Range, Yilgarn Craton, Western Australia. Chemical Geology 488,

124) Djokic, T., Van Kranendonk, M.J. (2018). Textural biosignatures from the Pilbara: An important benchmark for early life on Earth. PalZ. Paläontologische Zeitschrift,

123) Duda, J-P., Thiel, V., Bauersachs, T., Missbach, H., Reinhard, M., Schäfer, N., Van Kranendonk, M.J., Reitner, J. (2018): Ideas and perspectives: Hydrothermally driven redistribution and sequestration of early Archaean biomass—the ‘hydrothermal pump hypothesis’. Biogeosciences 15, 1535-1548.

122) Homann, M., Sansjofre, P., Van Zuilen, M., Heubeck, C., Gong, J., Killingsworth, B., Foster, I.S., Airo, A., Van Kranendonk, M.J., Ader, M., Lalonde, S.V., (2018): Microbial life and biogeochemical cycling on land 3,220 million years ago. Nature Geoscience 11, 665-671.

121) Otálora, F., Mazurier, A., García-Ruiz, J.M., Van Kranendonk, M.J., Kotopoulou, E., El Albani, A. and Garrido, C.J.  2018. A crystallographic study of crystalline casts and pseudomorphs from the 3.5 Ga Dresser Formation, Pilbara Craton (Australia). Journal of Applied Crystallography 51, 1050-1058.

120) Philippot, P., Ávila, J., Killingsworth, B., Baton, F., Tessalina, S., Caquineau, T., Muller, E., Pecoits, E., Cartigny, P., Lalonde, S., Ireland, T., Thomazo, C., Van Kranendonk, M., Busigny, V. (2018). Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event. Nature Communications 9, 2245; doi:10.1038/s41467-018-04621-x.

119) Smithies, R.H., Champion, D.C., Van Kranendonk, M.J. (2018): The oldest well-preserved felsic volcanic rocks on Earth: Geochemical clues to the early evolution of the Pilbara Supergroup and implications for the growth of a Paleoarchean protocontinent. In: Van Kranendonk, M.J., Bennett, V., Hoffmann, E. (eds.), Earth’s Oldest Rocks, 2nd Edition. Elsevier, USA.; p. 463-486.

118) Van Kranendonk, M.J., Djokic, T., Poole, G., Tadbiri, S., Steller, L., Baumgartner, R. (2018): Depositional setting of the fossiliferous, c. 3480 Ma Dresser Formation, Pilbara Craton: A review. In: Van Kranendonk, M.J., Bennett, V., Hoffmann, E. (eds.), Earth’s Oldest Rocks, 2nd Edition. Elsevier, USA; p. 985-1006.  

117) Van Kranendonk, M.J., Smithies, R.H., Champion, D.C. (2018): Paleoarchean development of a continental nucleus: the East Pilbara Terrane of the Pilbara Craton, Western Australia. In: Van Kranendonk, M.J., Bennett, V., Hoffmann, E. (eds.), Earth’s Oldest Rocks, 2nd Edition. Elsevier, USA.; p. 437-462.

2017 (4)

116) Djokic, T., Van Kranendonk, M.J., Campbell, K.A., Walter, M.R., Ward, C.R. (2017): Earliest signs of life on land preserved in c. 3.5 Ga hot spring deposits. Nature Communications 8:15263. DOI:10.1038/ncomms15263

115) Hwong, Y-L., Oliver, C., Van Kranendonk, M.J., Sammut, C., Seroussi, Y. (2017): What makes you tick? The psychology of social media engagement in space science communication. Computers in Human Behavior 68, 480-492.

114) Johnston, J.F., Van Kranendonk, M.J. (2017): A conversation about geology and tourism in a remote area of Australia. In: Dowling, R. and Newsome, D. (eds), Handbook of Geotourism. Edward Elgar Publishing, pp. 264-273.

113) Sugitani K, Oehler DZ, House CH, Walter MR (2017): Comment: Archean coastal-plain paleosols and life on land. Gondwana Research 44, 265-269.

2016 (11)

112) Barlow, E., Van Kranendonk, M.J. Yamaguchi, K.E., Ikehara, M., Lepland, A. (2016): Lithostratigraphic analysis of a new stromatolite-thrombolite reef from across the rise of atmospheric oxygen in the Paleoproterozoic Turee Creek Group, Western Australia. Geobiology 14, 317–343. DOI 10.1111/gbi.12175.

111) Duda, J-P., Van Kranendonk, M.J., Thief, V., Ionescu, D., Strauss, H., Schafer, N., Reitner, J. (2016): A rare glimpse of Paleoarchean life: Geobiology of an exceptionally preserved microbial mat facies from the 3.4 Ga Strelley Pool Formation, Western Australia. PlosOne 11(1). DOI 10.1371/journal.pone.0147629

110) Flannery, D.T., Allwood, A.C., Van Kranendonk, M.J. (2016): Lacustrine facies dependence of highly 13C-depleted organic matter during the Global Age of Methanotrophy. Precambrian Research 285, 216-241.

109) Gardiner, N.J., Kirkland, C.L., Van Kranendonk, M.J. (2016): More than Average: The Juvenile Hf Signal as a Record of Global Supercycles. Scientific Reports 6, 38503. DOI 10.1038/srep38503.

108) Herrero-Bervera, E., Krasa, D., Van Kranendonk, M.J. (2016): A whole rock absolute paleointensity determination of dacites from the Duffer Formation (ca. 3.467 Ga) of the Pilbara Craton, Australia: An impossible task? Physics of the Earth and Planetary Interiors 258, 51-62.

107) Morag, N., Williford, K.H., Kitajima, K., Philippot, P., Van Kranendonk, M.J., Lepot, K., Thomazo, C., Valley, J.W. (2016): Microstructure-specific carbon isotopic signatures of organic matter from ~3.5 Ga cherts of the Pilbara Craton support a biologic origin. Precambrian Research 275, 429-449.

106) Murphy, R.J., Van Kranendonk, M.J., Kelloway, S., Wainwright, I. (2016): Complex patterns in fossilised stromatolites revealed by hyperspectral imaging (400-2496 nm). Geobiology 14, 413-439. DOI 10.1111/gbi.12184

105) Nutman, A.P., Bennett, V.C., Friend, C.R.L., Van Kranendonk, M.J., Chivas, A. (2016): Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures. Nature 537, 535-538. DOI 10.1038/nature19355

104) Sossi, P.A., Eggins, S.M., Nesbitt, R.W., Nebel, O., Hergt, J.M., Campbell, I.H., O’Neill, H. St. C., Van Kranendonk, M.J., Davies, D.R. (2016): Petrogenesis and geochemistry of Archean komatiites. Journal of Petrology 57, 147-184. DOI 10.1093/petrology/egw004

103) Sugitani, K., Oehler, D., Van Kranendonk, M.J., House, C., Walter, M.R. (2016): Archean coastal-plain paleosols and life on land: Comment. Gondwana Research:

102) Van Kranendonk, M.J., Kirkland, C.L. (2016): Conditioned duality of the Earth System: Geochemical tracing of the supercontinent cycle through the Precambrian. Earth-Science Reviews 160, 171-187. DOI 10.1016/j.earscirev.2016.05.009

2015 (13)

101) Kurzweil, F., Wille, M., Schoenberg, R., Taubald, H., Van Kranendonk, M.J. (2015): Continuously increasing δ98Mo values in Neoarchean black shales and iron formations from the Hamersley Basin. Geochimica et Cosmochimica Acta 164, 523-542. DOI 10.1016/j.gca.2015.05.009

100) Martindale, R., Strauss, J.V., Sperling, E.A., Johnson, J.E., Van Kranendonk, M.J., Flannery, D.T., French, K., Lepot, K., Mazumder, R., Rice, M.S., Schrag, D.P., Summons, R., Walter, M., Abelson, J., Knoll, A.H. (2015): Sedimentology, chemostratigraphy, and stromatolites of lower Paleoproterozoic carbonates, Turee Creek Group, Western Australia. Precambrian Research 266, 194-211.

99) Mazumder, R., Van Kranendonk, M.J., Altermann, W. (2015): A marine to fluvial transition in the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia. Precambrian Research 258, 161-170.

98) Pagès, A., Grice, K., Welsh, D.T., Teasdale, P.T., Van Kranendonk, M.J., Greenwood, P.F. (2015): Lipid biomarker and isotopic study of community distribution and biomarker preservation in a laminated microbial mat from Shark Bay, Western Australia. Microbial Ecology 70, 459-472. DOI 10.1007/s00248-015-0598-3.

97) Roberts, N.M.W., Van Kranendonk, M.J., Parman, S., Clift, P. (2015): Continent Formation Through Time. In: Roberts, N.M.W., Van Kranendonk, M., Parman, S., Shirey, S. & Clift, P.D. (eds), Continent Formation Through Time. Geological Society, London, Special Publications 389, 1-16.

96) Schopf J.W., Kudryavtsev, A.B., Walter, M.R., Van Kranendonk, M.J., Williford, K.W., Kozdon, R., Valley, J.W., Gallardo, V.A., Espinoza, C., Flannery, D.T. (2015): Reply to Dvořák et al.: Apparent evolutionary stasis of ancient subseafloor sulfur cycling biocoenoses. Proceedings of the National Academy of Sciences 112 (20), E2560.

95) Schopf J.W., Kudryavtsev, A.B., Walter, M.R., Van Kranendonk, M.J., Williford, K.W., Kozdon, R., Valley, J.W., Gallardo, V.A., Espinoza, C., Flannery, D.T. (2015): A fossil sulfur-cycling microbiota from the 1.8 Ga Duck Creek Formation provides promising evidence of evolution's null hypothesis. Proceedings of the National Academy of Sciences 112, 2087-2092. DOI 10.1073/pnas.1419241112.

94) Sugitani, K., Mimura, K., Takeuchi, M., Yamaguchi, T., Suzuki, K., Senda, R., Asahara, Y., Van Kranendonk, M.J. (2015). A Paleoarchean coastal hydrothermal field inhabited by diverse microbial communities: the Strelley Pool Formation, Pilbara Craton, Western Australia. Geobiology 13, 522-545. DOI 10.1111/gbi.12150

93) Van Kranendonk, M.J., Mazumder, R. (2015): Two Paleoproterozoic glacio-eustatic cycles in the Turee Creek Group, Western Australia. Geological Society of America Bulletin 127, 596-607. DOI 10.1130/B31025.1

92) Van Kranendonk, M.J., Altermann, W., Mazumder, R. (2015): A squall by the seashore ca. 2.3 billion years ago: Raindrop imprints in a Paleoproterozoic tidal flat deposit, Kungarra Formation, Western Australia. Australian Journal of Earth Sciences 62, 265-274. DOI 10.1080/08120099.2015.1016105.

91) Van Kranendonk, M.J., Kirkland, C.L., Cliff, J. (2015): Oxygen isotopes in Pilbara Craton zircons support a global increase in crustal recycling at 3.2 Ga. Lithos 228-229, 90-98. doi:10.1016/j.lithos.2015.04.011

90) Van Kranendonk, M.J., Mazumder, R., Yamaguchi, K., Yamada, K., Ikehara, M. (2015): Sedimentology of the Paleoproterozoic Kungarra Formation, Turee Creek Group, Western Australia: A conformable record of the transition from early to modern Earth. Precambrian Research 256, 314-343. DOI 10.1016/j.precamres.2014.09.015

89) Van Kranendonk, M.J., Smithies, R.H., Griffin, W.L., Huston, D.L., Hickman, A.H., Champion, D.C., Anhaeusser, C.R., Pirajno, F. (2015): Making it thick: A volcanic plateau model for Paleoarchean continental lithosphere of the Pilbara and Kaapvaal cratons. In: Roberts, N.M.W., Van Kranendonk, M., Parman, S., Shirey, S. & Clift, P.D. (eds), Continent Formation Through Time. Geological Society, London, Special Publications 389, 83-112.

2014 (7)

88) Barnes, S., Van Kranendonk, M.J. (2014): Archean andesites in the East Yilgarn Craton, Western Australia: products of plume/crust interaction? Lithosphere 6, 80-92. DOI 10.1130/L356.1

87) Flannery, D.T., Van Kranendonk, M.J., Mazumder, R., Walter, M.R. (2014): The ~2.74 Ga Mopoke Member, Kylena Formation: a marine incursion into the northern Fortescue Group? Australian Journal of Earth Sciences 61, 1095-1108. DOI 10.1080/08120099.2014.960898

86) Hollis, J., Van Kranendonk, M.J., Cross, A., Kirkland, C.L., Armstrong, R.A. (2014): Low d18O zircon grains in the Neoarchean Rum Jungle Complex, northern Australia: an indicator of emergent continental crust. Lithosphere 6, 17–25.

85) Nebel, O., Campbell, I.H., Sossi, P.A., Van Kranendonk, M.J. (2014): Hafnium and iron isotopes in early Archean komatiites record a plume-driven convection cycle in the Hadean Earth. Earth and Planetary Science Letters 397, 111-120. DOI 10.1016/j.epsl.2014.04.028

84) Ushikubo, T., Williford, K.H., Farquhar, J., Johnston, D.T., Van Kranendonk, M.J., Valley, J.W. (2014): Development of in situ sulfur four-isotope analysis with multiple Faraday cup detectors by SIMS and application to pyrite grains in a Paleoproterozoic glaciogenic sandstone. Chemical Geology 383, 86-99. DOI 10.1016/j.chemgeo.2014.06.006

83) Van Kranendonk, M.J. (2014): Early Earth atmosphere and environments: A review. In: Shaw, G.H. (ed.), Earth’s Early Atmosphere and Surface Environment. Geological Society of America, Special Papers 504, 105-130.

82) Van Kranendonk, M.J., Kröner, A., Hoffman, J.E., Nagel, T., Anhaeusser, C.R. (2014): Just another drip: Re-analysis of a proposed Mesoarchean suture from the Barberton Mountain Land. Precambrian Research 54, 19-35. DOI 10.1016/j.precamres.2014.07.022.

2013 (5)

81) Li, W., Czaja, A.D., Van Kranendonk, M.J., Beard, B.L., Roden, E.E., Johnson, C.M. (2013): An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago. Geochimica et Cosmochimica Acta 120, 65–79. DOI 10.1016/j.gca.2013.06.033.

80) Mazumder, R., Van Kranendonk, M.J. (2013): Palaeoproterozoic terrestrial sedimentation in the Beasley River Quartzite, lower Wyloo Group, Western Australia. Precambrian Research 231, 98–105.

79) Van Kranendonk, M.J., Kirkland, C.L. (2013): Orogenic climax of Earth: the 1.2–1.1 Ga Grenvillian Superevent. Geology 41, 735–738. DOI 10.1130/G34243.1

78) Van Kranendonk, M.J., Ivanic, T.J., Wingate, M.T.D., Kirkland, C.L., Wyche, S. (2013): Long-lived, autochthonous development of the Archean Murchison Domain, Yilgarn Craton, and implications for Yilgarn Craton tectonics. Precambrian Research 229, 49–92.

77) Wille, M., Nebel, O., Van Kranendonk, M.J., Schoenberg, R., Kleinhanns, I., Ellwood, M.J. (2013): Mo-Cr isotope evidence for a reducing Archean atmosphere in 3.46–2.76 Ga black shales from Pilbara, Western Australia. Chemical Geology 340, 68–76.

2012 (4)

76) Barnes, S., Van Kranendonk, M.J., Sontag, I. (2012): Geochemistry and tectonic setting of basalts from the Eastern Goldfields Superterrane. Australian Journal of Earth Sciences 59, 707–735.

75) Hickman, A.H., Van Kranendonk, M.J. (2012): Early Earth evolution: evidence from the 3.5–1.8 Ga geological history of the Pilbara region of Western Australia. Episodes 35, 283–297.

74) Ivanic, T.J., Van Kranendonk, M.J., Kirkland, C.L., Wyche, S., Wingate, M.T.D., Belousova, E.A. (2012): Zircon Lu–Hf isotopes and granite geochemistry of the Murchison Domain of the Yilgarn Craton: Evidence for reworking of Eoarchean crust during Meso-Neoarchean plume-driven magmatism. Lithos 148, 112–127.

73) Van Kranendonk, M.J., Altermann, W., Beard, B.L., Hoffman, P.F., Johnson, C.J., Kasting, J.F., Melezhik, V.A., Nutman, A.P., Papineau, D., and Pirajno, F. (2012): A chronostratigraphic division of the Precambrian: possibilities and challenges. In: Gradstein, F.M, Ogg, J.G., Schmitz, M.D., Ogg, G.J. (eds.), The Geologic Time Scale 2012; Elsevier, Boston, USA, pp. 299–392.

2011 (4)

72) Williford, K.H., Van Kranendonk, M.J., Ushikubo, T., Kozdon, R., Valley, J.W. (2011): Constraining atmospheric oxygen and seawater sulfate concentrations during Paleoproterozoic glaciation: in situ sulfur three-isotope microanalysis of pyrite from the Turee Creek Group, Western Australia. Geochimica et Cosmochimica Acta 75, 5686–5705.

71) Van Kranendonk, M.J. (2011): Onset of plate tectonics. Science 333, 413–414.

70) Van Kranendonk, M.J. (2011): Cool greenstone drips, hot rising domes, and the role of partial convective overturn in Barberton greenstone belt evolution.Journal of African Earth Sciences 60, 346–352. DOI: 10.1016/j.jafrearsci.2011.03.012.

69) Van Kranendonk, M.J. (2011): Stromatolite morphology as an indicator of biogenicity for Earth’s oldest fossils from the 3.5-3.4 Ga Pilbara Craton, Western Australia. In:Advances in Stromatolite Geobiology, edited by J. Reitner, N-V. Queric, and G. Arp.Lecture Notes in Earth Sciences, v. 131, Spiinger, Germany, pp. 517–534.

68) Ivanic, T.J., Wingate, M.T.D., Kirkland, C.L., Van Kranendonk, M.J., Wyche, S. (2010): Age and significance of voluminous mafic–ultramafic magmatic events in the Murchison Domain, Yilgarn Craton. Australian Journal of Earth Sciences57, 597–614.

67) Kirkland, C.L., Whitehouse, M.J., Pease, V., and Van Kranendonk, M.J., 2010b, Erratum: Lithosphere, v. 2, p. 472–475.

66)Kirkland, C.L., Whitehouse, M.J., Pease, V., Van Kranendonk, M.J. (2010): Oxygen isotopesin detrital zircons: Insight into crustal recycling during the evolution of the Greenland Shield.Lithosphere 2, 3-12.

65) Sugitani, K., Lepot, K., Mimura, K., Van Kranendonk, M.J., Oehler, D., Walter, M.R. (2010): Biogenicity of morphologically diverse carbonaceous microstructures from the ca. 3400 Ma Strelley Pool Formation, in the Pilbara Craton, Western Australia. Astrobiology 10, 899–920.

64) Tessalina, S.G., Bourdon, B., Van Kranendonk, M., Birck, J-L., Philippot, P. (2010): Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton. Nature Geoscience 3, 214-217.

63) Van Kranendonk, M.J. (2010): Two types of Archean continental crust: plumeand plate tectonics on early Earth. American Journal of Science 310, 1187–1209DOI: 10.2475/10.2010.01

62) Van Kranendonk, M.J., Smithies, R.H., Hickman, A.H., Wingate, M.T.D., Bodorkos, S. (2010): Evidence for Mesoarchean (~3.2 Ga) rifting of the Pilbara Craton: The missing link in an early Precambrian Wilson cycle. Precambrian Research 177, 145-161.

61) Gérard, E., Moreira, D., Philippot, P., Van Kranendonk, M., López-Garcia, P. (2009): Modern subsurface bacteria in pristine 2.7 Ga-old fossil stromatolite drillcore samples from the Fortescue Group, Western Australia. PLoS ONE4(4): e5298. (doi:10.1371/journal.pone.0005298).

60) Philippot, P., Van Kranendonk, M., Van Zuilen, M. Lepot, K., Rividi, N., Teitler, Y., Thomazo, C., Blanc-Valleron, M-M., Rouchy, J-M., Grosch, E., de Wit, M. (2009): Early traces of life investigations in drilling Archean hydrothermal and sedimentary rocks of the Pilbara Craton, Western Australia and Barberton Greenstone Belt, South Africa. C. R. Palevol 8, 649-663.

59) Smithies, R.H. Champion, D. C., Van Kranendonk, M. J. (2009): Formation of Paleoarchean continental crust through infracrustal melting of enriched basalt.Earth and Planetary Science Letters 281, 298-306 (doi: 10.1016/j.epsl.2009.03.003).

58) Van Kranendonk, M.J., Kröner, A., Hegner, E., Connelly, J. (2009): Age, lithology and structural evolution of the c. 3.53 Ga Theespruit Formation in the Tjakastad area, southwestern Barberton Greenstone Belt, South Africa, with implications for Archean tectonics. Chemical Geology 261, 114-138.

57) Furnes, H., McLoughlin, N. Muehlenbachs, K., Banerjee, N.R., Staudigel, H., Dilek, Y., de Wit, M., Van Kranendonk, M., Schiffman, P. (2008): Oceanic pillow lavas and hyaloclastites as habitats for microbial life through time – A review. In: Dilek, Y., Furnes, H., Muehlenbachs, K. (eds.), Links between geological processes, microbial activities and evolution of life. Springer-Verlag Book Series, pp. 1-68.

56) McLoughlin, N., Furnes, H., Banerjee, N.R., Staudigel, H., Muehlenbachs, K., de Wit, M., Van Kranendonk, M. (2008): Micro-bioerosion in volcanic glass: Extending the ichnofossil record to Archean basaltic crust. In: Wisshak, M. and Tapinla, L. (eds.), Current Developments in Bioerosion. Springer, Berlin, pp. 372-396.

55) Pease, V., Percival, J., Smithies, R. H., Stevens, G.,Van Kranendonk, M.J.(2008): When did plate tectonics begin? Evidence from the orogenic record. In: Condie, K.C. and Pease, V. (eds.), When did plate tectonics begin on Earth? Geological Society of America, Special Paper 440, p. 199-228.

54) Philippot, P., Van Zuilen, M., Lepot, K., Thomazo, C., Farquhar, J., Van Kranendonk, M. (2008): Response to comment on “Early Archean microorganisms preferred elemental sulphur, not sulphate”. Science, v. 319, p. 1336c-1336d.

53) Pirajno, F.,Van Kranendonk, M.J., Xiao, L. (2008): Hydrothermal processes in the solar system: A review. Geological Science and Technology Information, v. 27(1), p. 1–12.

52) Thébaud, N., Philippot, P., Rey, P., Brugger, J.,Van Kranendonk, M., Grassineau, N. (2008): Protracted fluid-rock interaction in the Mesoarchaean and implication for gold mineralization: Example from the Warrawoona Syncline (Pilbara, Western Australia). Earth and Planetary Science Letters, v. 272, p. 639-655.

51) Van Kranendonk, M.J., Gehling, J., Shields, G. (2008): Precambrian. In: Ogg, J.G., Ogg, G., Gradstein, F. (eds.), The Concise Geological Timescale, p. 23-36. Cambridge University Press.

50) Van Kranendonk, M.J., Philippot, P., Lepot, K., Bodorkos, S., Pirajno, F. (2008): Geological setting of Earth’s oldest fossils in the c. 3.5 Ga Dresser Formation, Pilbara Craton, Western Australia. Precambrian Research 167, 93-124. doi. 10.1016/j.precamres.2008.07.003.

49) Banerjee, N. R., Simonnetti, A., Furnes, H., Muehlenbachs, K., Staudigel, H., Heaman, L., Van Kranendonk, M.J. (2007): Direct dating of Archean microbial ichnofossils. Geology, v. 35, p. 487-490.

48) Bolhar, R., Van Kranendonk, M.J. (2007): A non-marine depositional setting for the northern Fortescue Group, Pilbara Craton, inferred from trace element geochemistry of stromatolitic carbonates.Precambrian Research, v. 155, p. 229-250.

47) Furnes, H., Banerjee, N. R., Staudigel, H., Muehlenbachs, K., de Wit, M., Van Kranendonk, M.(2007): Comparing petrographic signatures of bioalteration in recent to Mesoarchean pillow lavas: Tracing subsurface life in oceanic igneous rocks. Precambrian Research, v. 158, p. 156-176.

46) Marshall, C.P., Love, G.D., Snape, C.E., Hill, A.C., Allwood, A.C., Walter, M.R.,Van Kranendonk, M.J., Bowden, S.A., Sylva, S.P., Summons, R.E. (2007): Structural characterization of kerogen in 3.4 Ga Archaean cherts from the Pilbara Craton, Western Australia. Precambrian Research, v. 155, p. 1-23.

45) Philippot, P., Van Zuilen, M., Lepot, K., Thomazo, C., Farquhar, J., Van Kranendonk, M. (2007): Early Archean microorganisms preferred elemental sulphur, not sulphate. Science, v. 317, p. 1534-1537.

44) Smithies, R.H., Champion, D.C.,Van Kranendonk, M.J. (2007): The oldest well-preserved volcanic rocks on Earth: geochemical clues to the early evolution of the Pilbara Supergroup and implications for the growth of a Paleoarchean continent. In: Van Kranendonk, M. J., Smithies, R. H., and Bennet, V. (Eds.),Earth’s Oldest Rocks. Developments in Precambrian Geology 15, p. 339-367. Elsevier, Amsterdam.

43) Smithies, R.H., Van Kranendonk, M.J., Champion, D.C., (2007): The Mesoarchaean emergence of modern style subduction. In: S. Maruyama and M. Santosh (eds.), Island Arcs: Past and Present; Gondwana Research, v. 11, p. 50-68.

42) Sugitani, K., Grey, K., Allwood, A.C., Nagaoka, T., Minami, M., Marshall, C.P.,Van Kranendonk, M.J., Walter, M.R. (2007): Diverse microstructures from Archean chert from the Mount Goldsworthy – Mount Grant area, Pilbara Craton, Western Australia: Microfossils, dubiofossils, or pseudofossils? Precambrian Research, v. 158, p. 228-262.

41) Van Kranendonk, M.J. (2007): Tectonics of early Earth; In: Van Kranendonk, M. J., Smithies, R. H., and Bennet, V. (Eds.), Earth’s Oldest Rocks. Developments in Precambrian Geology 15, p. 1105-1116. Elsevier, Amsterdam.

40) Van Kranendonk, M.J. (2007): A review of the evidence for putative Paleoarchean life in the Pilbara Craton.In: Van Kranendonk, M. J., Smithies, R. H., and Bennet, V. (Eds.), Earth’s Oldest Rocks. Developments in Precambrian Geology 15, p. 855-896. Elsevier, Amsterdam.

39) Van Kranendonk, M.J., Hickman, A., Smithies, R. H. (2007): The East Pilbara Terrane of the Pilbara Craton, Western Australia: Formation of a continental nucleus through repeated mantle plume magmatism; In: Van Kranendonk, M. J., Smithies, R. H., and Bennet, V. (Eds.), Earth’s Oldest Rocks. Developments in Precambrian Geology 15, p. 307-337. Elsevier, Amsterdam.

38) Van Kranendonk, M.J., Smithies, R.H., Hickman, A.H., Champion, D.C. (2007): Secular tectonic evolution of Archaean continental crust: interplay between horizontal and vertical processes in the formation of the Pilbara Craton, Australia. Terra Nova, v. 19(1), p. 1-38.

37) Van Kranendonk, M.J. (2006): Volcanic degassing, hydrothermal circulation and the flourishing of early life on Earth: new evidence from the Warrawoona Group, Pilbara Craton, Western Australia. Earth-Science Reviews, v. 74, p. 197-240.

36) Van Kranendonk, M.J., Bleeker, W., Ketchum, J. (2006): Phreatomagmatic boulder conglomerates at the fracture propagation tip of the 2.77 Ga Black Range dolerite dyke, Pilbara Craton, Western Australia. Australian Journal of Earth Sciences, v. 53, p. 617-630.

35) Bolhar, R., Van Kranendonk, M.J., Kamber, B.S. (2005): A trace element study of siderite-jasper banded iron formation in the 3.45 Ga Warrawoona Group, Pilbara Craton – formation from hydrothermal fluids and shallow seawater. Precambrian Research, v. 137, p. 93-114.

34) Pirajno, F., Van Kranendonk, M.J. (2005): A review of hydrothermal processes and systems on earth and implications for Martian analogues.Australian Journal of Earth Sciences, v. 52, p. 329-351.

33) Smithies, R.H., Champion, D.C., Van Kranendonk, M.J., Howard, H.M., Hickman, A.H. (2005a): Modern-style subduction processes in the Mesoarchaean: geochemical evidence from the 3.12 Ga Whundo intraoceanic arc. Earth and Planetary Science Letters, v. 231, p. 221-237.

32) Smithies, R.H., Van Kranendonk, M.J., Champion, D.C. (2005b): It started with a plume – early Archaean basaltic proto-continental crust.Earth and Planetary Science Letters, v. 238 (3-4), p. 284-297.

31) Hickman, A.H., Van Kranendonk, M.J. (2004): Diapiric processes in the formation of Archaean continental crust, East Pilbara Granite-Greenstone Terrane, Australia. In: Eriksson, P.G., Altermann, W., Nelson, D.R., Mueller, W.U., Catuneau, O. (eds.), The Precambrian Earth: Tempos and Events. Elsevier, p. 54-75.

30) Pawley, M.J., Van Kranendonk, M.J., Collins, W.J. (2004):Interplay between deformation and magmatism during doming of the Archaean Shaw Granitoid Complex, Pilbara Craton, Western Australia.Precambrian Research, v. 131, p. 213-230.

29) Sandiford, M., Van Kranendonk, M.J., Bodorkos, S. (2004): Conductive incubation and the origin of dome-and-keel structure in Archean granite-greenstone terrains: a model based on the eastern Pilbara Craton, Western Australia. Tectonics23, TC1009, DOI: 10.1029/2002TC001452.

28) Van Kranendonk, M.J., (2004): Archaean tectonics 2004: A review.Precambrian Research, v. 131, p. 143-151. doi: 10.1016/j.precamres.2003.12.008

27) Van Kranendonk, M.J., Cassidy, K. (2004): Comment on: “An Alternative Earth”. GSA Today, v. 14, no. 3, p. 14.

26) Van Kranendonk, M.J., Pirajno, F. (2004): Geological setting and geochemistry of metabasalts and alteration zones associated with hydrothermal chert ± barite deposits in the ca. 3.45 Ga Warrawoona Group, Pilbara Craton, Australia. Geochemistry: Exploration, Environment, Analysis, v. 4, p. 253-278.

25) Van Kranendonk, M.J., Collins, W.J., Hickman, A.H., Pawley, M.J. (2004): Critical tests of vertical vs horizontal tectonic models for the Archaean East Pilbara Granite-Greenstone Terrane, Pilbara Craton, Western Australia.Precambrian Research, v. 131, p. 173-211.

24) Garcia-Ruiz J.M., Hyde, S.T., Carnerup, A.M., Christy, A.G., Van Kranendonk, M.J., Welham, N.J. (2003): Self-assembled silica-carbonate structures and detection of ancient microfossils. Science, v. 302, p. 1194-1197.

23) Van Kranendonk, M.J. (2003): Archaean tectonics in 2001: An Earth odyssey.Precambrian Research, v. 127(1-3), p. 1-4.

22) Van Kranendonk, M.J., Webb, G. E., Kamber, B.S. (2003):Geological and trace element evidence for a marine sedimentary environment of deposition and biogenicity of 3.45 Ga stromatolitic carbonates in the Pilbara Craton, and support for a reducing Archean ocean. Geobiology, v. 1(2), p. 91-108.

21) Brasier, M.D., Green, O.R., Jephcoat, A.P., Kleppe, A.K., Van Kranendonk, M.J., Lindsay, J.F., Steele, A., Grassineau, N. (2002): Questioning the evidence for Earth's oldest fossils. Nature, v. 416, p. 76-81.

20) Huston, D.L., Sun, S-S, Blewett, R.H., Hickman, A.H., Van Kranendonk, M.J.,Phillips, D., Baker, D., Brauhart, C. (2002): The timing of mineralization in the Archaean North Pilbara Terrain, Western Australia. Economic Geology, v. 97 (4),p. 733-756.

19) Pawley, M., Collins, W.J., Van Kranendonk, M.J. (2002): Origin of fine-scale sheeted granites by incremental injection of magma into active shear zones: examples from the Pilbara Craton, NW Australia. Lithos, v. 61 (3-4), p. 127-139.

18) Van Kranendonk, M.J., Hickman, A.H., Smithies, R.H., Nelson, D.N., Pike, G. (2002): Geology and tectonic evolution of the Archaean North Pilbara terrain, Pilbara Craton, Western Australia. Economic Geology, v. 97 (4), p. 695-732.

17) Van Kranendonk, M.J., Hickman, A.H., Collins, W.J. (2001): Comment on “Evidence for multiphase deformation in the Archaean basal Warrawoona Group in the Marble Bar area, East Pilbara, Western Australia”. Precambrian Research,v. 105, p. 73-78.

16) Collins, W.J., Van Kranendonk, M.J. (1999): Model for the development of kyanite during partial convective overturn of Archaean granite-greenstone terranes: the Pilbara Craton, Australia. Journal of Metamorphic Geology, v. 17, No. 2, p. 145-156.

15) Collins, W.J., Van Kranendonk, M.J., Teyssier, C. (1998): Partial convective overturn of Archaean crust in the east Pilbara Craton, Western Australia: Driving mechanisms and tectonic implications. Journal of Structural Geology, v. 20, p. 1405-1424.

14) Van Kranendonk, M.J., Collins, W.J. (1998): Timing and tectonic significance of Late Archaean, sinistral strike-slip deformation in the Central Pilbara Structural Corridor, Pilbara Craton, Western Australia. Precambrian Research, v. 88, p. 207-232.

13) Van Kranendonk, M.J., Wardle, R.J. (1997): Crustal-scale flexural slip folding during late tectonic amplification of an orogenic boundary perturbation in the Paleoproterozoic Torngat Orogen, NE Canada. Canadian Journal of Earth Sciences, v. 34, p. 1545-1565.

12) Van Kranendonk, M.J., Wardle, R.J. (1996): Burwell domain of the Paleoproterozoic Torngat Orogen, northeastern Canada: Tilted cross-section of a magmatic arc caught between a rock and a hard place. In: Brewer, T.S. (ed.) Precambrian evolution of the North Atlantic Region; Geological Society Special Publication No. 112, p. 91-115.

11) Wardle, R.J., Van Kranendonk, M.J. (1996): The Eastern Churchill Province of Labrador-Québec, Canada: Orogenic development as a consequence of oblique collision and indentation. In: Brewer, T.S. (ed.) Precambrian Evolution of the North Atlantic Region; Geological Society of London, Special Publication No. 112, p. 137-153.

10) Van Kranendonk, M.J. (1996): Tectonic evolution of the Paleoproterozoic Torngat Orogen; Evidence from P-T-t-d paths in the North River map area, Labrador. Tectonics, v. 15, No. 4, p. 843-869.

9) Van Kranendonk, M.J., St-Onge, M.R., Henderson, J.R. (1993): Paleoproterozoic tectonic assembly of Northeast Laurentia through multiple indentations. Precambrian Research, v. 63, p. 325-347.

8) Bertrand, J.-M., Roddick, J.C., Van Kranendonk, M.J., Ermanovics, I. (1993): U-Pb geochronology of deformation and metamorphism in the Early Proterozoic Torngat Orogen, North River map area, Labrador. Canadian Journal of Earth Sciences, v. 30, p. 1470-1489.

7) Van Kranendonk, M.J., Helmstaedt, H. (1992): Late Archean structural history of allochthonous Upernavik supracrustal rocks in the high-grade Nain Province, Labrador: Evidence of a link between the tectonic evolution of gneiss terranes and greenstone belts. In: Glover, J.E. and Ho, S.E. (editors) The Archaean: Terrains, Processes and Metallogeny, p. 137-149. Geology Department (Key Centre) and University Extension, The University of Western Australia, Publication No. 22, 1992.

 6) Van Kranendonk, M.J. (1991): A magmatic sheet origin for thin metagabbroic anorthosite units in the Fishog subdomain of the southern Central Gneiss Belt, Grenville Province, Ontario. Canadian Journal of Earth Sciences, v. 28, p. 431-446.

5) Van Kranendonk, M.J., Ermanovics, I. (1990): Structural evolution of the Hudsonian Torngat Orogen in the North River map area, Labrador. Geoscience Canada, v.17, no.4, p. 283-288.

4) Van Kranendonk, M.J., Helmstaedt, H. (1990): Late Archean geological history of the Nain Province, North River-Nutak map area, Labrador and its tectonic significance. Geoscience Canada, v.17, no.4, p.231-237.

3) Bertrand, J.-M., Van Kranendonk, M., Hanmer, S., Roddick, J.C., Ermanovics, I. (1990): Structural and metamorphic geochronology of the Torngat Orogen, Labrador: Preliminary results. Geoscience Canada, v.17, no.4, p.297-301.

2) Ermanovics, I., Van Kranendonk, M. (1990): The Nutak - North River transect of Nain and Churchill (E. Rae Terrane) Provinces: the Torngat Orogen. Geoscience Canada, v.17, no.4, p.279-283.

 1) Schwerdtner, W.M., Van Kranendonk, M. (1984): Structure of Stolz diapir ? a well?exposed salt dome on Axel Heiberg Island, Canadian Arctic Archipelago.Bull. Can. Petroleum Geology, v.  32, p. 237?241


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