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Journal articles on the topic 'Geology, Stratigraphic – Archaean'

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1

van Loon, A. J., R. Mazumder, and S. De. "Unravelling the depositional environment of the Archaean Rajkharsawan conglomerate (Jharkhand, eastern India)." Netherlands Journal of Geosciences - Geologie en Mijnbouw 91, no. 1-2 (2012): 129–35. http://dx.doi.org/10.1017/s0016774600001542.

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AbstractLarge conglomerate lenses occur in a fine-grained siliciclastic succession of the Singhbhum craton, eastern India. They overlie an Archaean orthogneiss, from which they are separated by a palaeosol. Neither the conglomerates nor the directly overlying rocks have been dated, but the conglomerate unit is assumed to have also an Archaean age. The conglomerate lenses occur within a succession of pelitic and mafic schists, and the depositional environment of this conglomerate/schist unit had not been clarified thus far. On the basis of a combination of the vertical and horizontal distributi
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2

Hicks, N., and D. J. C. Gold. "A reinterpretation of the Archaean stratigraphy south of Nkandla, southern Kaapvaal Craton, South Africa: Geophysical and stratigraphic constraints on a sheared granitoid-greenstone remnant." South African Journal of Geology 124, no. 3 (2021): 685–98. http://dx.doi.org/10.25131/sajg.124.0025.

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Abstract A new lithostratigraphic framework based upon a review of historic data, field mapping and remote sensing, including aerial photography, high-resolution airborne aeromagnetic and radiometric data, is proposed for the Archaean geology along the southeastern margin of the Kaapvaal Craton, South Africa. A synthesis of new and existing data reveals that previously accepted lithostratigraphic schemes require complete revision, with reinterpretations identifying multiple major shear zones and previously unidentified granitoid successions along the margin of the craton. In this new lithostra
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3

Hickman-Lewis, K., and F. Westall. "A southern African perspective on the co-evolution of early life and environments." South African Journal of Geology 124, no. 1 (2021): 225–52. http://dx.doi.org/10.25131/sajg.124.0016.

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Abstract The Kaapvaal and Zimbabwe cratons host some of the earliest evidence for life. When compared to the contemporaneous East Pilbara craton, cherts and other metasedimentary horizons in southern Africa preserve traces of life with far greater morphological and geochemical fidelity. In spite of this, most fossiliferous horizons of southern Africa have received relatively limited attention. This review summarises current knowledge regarding the nature of early life and its distribution with respect to environments and ecosystems in the Archaean (>2.5 Ga) of the region, correlating st
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4

Friend, C. R. L., and A. P. Nutman. "Tectono-stratigraphic terranes in Archaean gneiss complexes as evidence for plate tectonics: The Nuuk region, southern West Greenland." Gondwana Research 72 (August 2019): 213–37. http://dx.doi.org/10.1016/j.gr.2019.03.004.

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5

MARTIN, D. McB, C. W. CLENDENIN, B. KRAPEZ, and N. J. McNAUGHTON. "Tectonic and geochronological constraints on late Archaean and Palaeoproterozoic stratigraphic correlation within and between the Kaapvaal and Pilbara Cratons." Journal of the Geological Society 155, no. 2 (1998): 311–22. http://dx.doi.org/10.1144/gsjgs.155.2.0311.

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6

Kenny, Gavin G., Gary J. O’Sullivan, Stephen Alexander, Michael J. Simms, David M. Chew, and Balz S. Kamber. "On the track of a Scottish impact structure: a detrital zircon and apatite provenance study of the Stac Fada Member and wider Stoer Group, NW Scotland." Geological Magazine 156, no. 11 (2019): 1863–76. http://dx.doi.org/10.1017/s0016756819000220.

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AbstractThe Stac Fada Member of the Stoer Group, within the Torridonian succession of NW Scotland, is a melt-rich, impact-related deposit that has not been conclusively correlated with any known impact structure. However, a gravity low approximately 50 km east of the preserved Stac Fada Member outcrops has recently been proposed as the associated impact site. We investigate the location of the impact structure through a provenance study of detrital zircon and apatite in five samples from the Stoer Group. Our zircon U–Pb data are dominated by Archaean grains (> 2.5 Ga), consistent with earli
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7

Yu, Hongchao, Jin Liu, Zhonghua He, et al. "Geochronology and Zircon Hf Isotope of the Paleoproterozoic Gaixian Formation in the Southeastern Liaodong Peninsula: Implication for the Tectonic Evolution of the Jiao-Liao-Ji Belt." Minerals 12, no. 7 (2022): 792. http://dx.doi.org/10.3390/min12070792.

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The Jiao-Liao-Ji belt (JLJB), in the Eastern Block of the North China Craton, is a major Paleoproterozoic orogen and underwent a complicated tectonic evolution during 2.2–1.8 Ga. The Liaohe Group, an important stratigraphic unit in the JLJB, is key to understanding the complex evolution of this belt. In this paper, we present new detrital zircon U–Pb ages and Hf isotope data for meta-sedimentary rocks from the Gaixian Formation in different areas of the JLJB, in addition to compiled data for other formations of the Liaohe Group, to establish the depositional age and source of detrital material
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8

JASTRZĘBSKI, MIROSŁAW, ANDRZEJ ŻELAŹNIEWICZ, IZABELLA NOWAK, MENTOR MURTEZI, and ALEXANDER N. LARIONOV. "Protolith age and provenance of metasedimentary rocks in Variscan allochthon units: U–Pb SHRIMP zircon data from the Orlica–Śnieżnik Dome, West Sudetes." Geological Magazine 147, no. 3 (2009): 416–33. http://dx.doi.org/10.1017/s0016756809990501.

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AbstractNew U–Pb sensitive high-mass resolution ion microprobe (SHRIMP) data from detrital zircons within the Orlica–Śnieżnik Dome provide new insights into the stratigraphic and palaeogeographic position of assumed relict Precambrian basement preserved in the Variscan collisional orogen of the West Sudetes, SW Poland. Hitherto, the Młynowiec Formation and the Stronie Formation within the Orlica–Śnieżnik Dome were assumed to represent two metavolcano-sedimentary successions of Proterozoic and early Palaeozoic age, respectively. However, when previous U–Pb data and mapping data from the Orlica–
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9

Higgins, A. K. "Geology of central and eastern North Greenland." Rapport Grønlands Geologiske Undersøgelse 128 (December 31, 1986): 37–54. http://dx.doi.org/10.34194/rapggu.v128.7923.

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A historical review of geological research in North Greenland is followed by a summary of the main results of the 1978-80 GGU expeditions to the region. New outcrops of Archaean and early Proterozoic crystalline rocks are recorded only as xenoliths in dykes and volcanic centres. A revised stratigraphy is applied to the middle Proterozoic Independence Fjord Group sandstones, while petrographic and isotopic studies have been made of the cross-cutting Midsommersø dolerites and the overlying Zig-Zag Dal Basalt Formation. No convincing evidence has been found of a Carolinidian orogenic episode sepa
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10

Wilks, M. E., and E. G. Nisbet. "Stratigraphy of the Steep Rock Group, northwest Ontario: a major Archaean unconformity and Archaean stromatolites." Canadian Journal of Earth Sciences 25, no. 3 (1988): 370–91. http://dx.doi.org/10.1139/e88-040.

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The Archaean Steep Rock Group of northwest Ontario, situated in the Wabigoon Subprovince of the Superior Province, Canada, comprises five formations: Wagita Formation (clastics), Mosher Carbonate, Jolliffe Ore Zone, Dismal Ashrock, and Witch Bay Formation (metavolcanics). Reinvestigation of the geology of the group has shown that the basal clastics of the Wagita Formation (0–150 m) unconformably overlie the Marmion Complex (a massive tonalite – tonalite gneiss terrane, 3 Ga old). Overlying the basal elastics is the Mosher Carbonate (0–500 m), containing diverse stromatolite morphologies. Exten
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11

Catuneanu, Octavian. "Flexural partitioning of the Late Archaean Witwatersrand foreland system, South Africa." Sedimentary Geology 141-142 (June 2001): 95–112. http://dx.doi.org/10.1016/s0037-0738(01)00070-7.

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12

Mueller, W. U., and P. L. Corcoran. "Late-orogenic basins in the Archaean Superior Province, Canada: characteristics and inferences." Sedimentary Geology 120, no. 1-4 (1998): 177–203. http://dx.doi.org/10.1016/s0037-0738(98)00032-3.

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13

van der Westhuizen, W. A., N. J. Grobler, J. C. Loock, and E. A. W. Tordiffe. "Raindrop imprints in the Late Archaean-Early Proterozoic Ventersdorp Supergroup, South Africa." Sedimentary Geology 61, no. 3-4 (1989): 303–9. http://dx.doi.org/10.1016/0037-0738(89)90064-x.

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14

Svetova, A. I., and S. A. Svetov. "The stratigraphical boundary between the lower and upper Lopian (upper Archaean) in central Karelia." GFF 118, sup004 (1996): 27. http://dx.doi.org/10.1080/11035899609546296.

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15

Els, B. G. "The auriferous late Archaean sedimentation systems of South Africa: unique palaeo-environmental conditions?" Sedimentary Geology 120, no. 1-4 (1998): 205–24. http://dx.doi.org/10.1016/s0037-0738(98)00033-5.

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16

DiMARCO, MICHAEL J., and DONALD R. LOWE. "Petrography and provenance of silicified early Archaean volcaniclastic sandstones, eastern Pilbara Block, Western Australia." Sedimentology 36, no. 5 (1989): 821–36. http://dx.doi.org/10.1111/j.1365-3091.1989.tb01748.x.

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17

Donaldson, J. Allan, and Eric A. de Kemp. "Archaean quartz arenites in the Canadian Shield: examples from the Superior and Churchill Provinces." Sedimentary Geology 120, no. 1-4 (1998): 153–76. http://dx.doi.org/10.1016/s0037-0738(98)00031-1.

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18

Krapez, Bryan. "Sequence stratigraphy of the Archaean supracrustal belts of the Pilbara Block, Western Australia." Precambrian Research 60, no. 1-4 (1993): 1–45. http://dx.doi.org/10.1016/0301-9268(93)90043-2.

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19

Henriksen, N., J. D. Friderichsen, R. A. Strachan, N. J. Soper, and A. K. Higgins. "Caledonian and pre-Caledonian geology of the region between Grandjean Fjord and Bessel Fjord (75°–76°N), North-East Greenland." Rapport Grønlands Geologiske Undersøgelse 145 (December 31, 1989): 90–97. http://dx.doi.org/10.34194/rapggu.v145.8084.

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The area between Grandjean Fjord and Bessel Fjord was the focus in 1988 of regional geological investigations and 1:500000 mapping during the North-East Greenland project (Henriksen, 1989). The greater part of the area forms part of the East Greenland Caledonides and can be divided into three distinct rock groups: infracrustal gneisses and granites of possibie Archaean or early Proterozoic origin; a metasedimentary sequence which has probably suffered both mid-Proterozoic and Caledonian migmatisation and metamorphism; and the late Proterozoic Eleonore Bay Group, a thick sedimentary sequence wh
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20

Toulkeridis, Theofilos, Norbert Clauer, Alfred Kröner, Thomas Reimer, and Wolfgang Todt. "Characterization, provenance, and tectonic setting of Fig Tree greywackes from the Archaean Barberton Greenstone Belt, South Africa." Sedimentary Geology 124, no. 1-4 (1999): 113–29. http://dx.doi.org/10.1016/s0037-0738(98)00123-7.

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21

RING, UWE, HILDE L. SCHWARTZ, TIMOTHY G. BROMAGE, and CHARLES SANAANE. "Kinematic and sedimentological evolution of the Manyara Rift in northern Tanzania, East Africa." Geological Magazine 142, no. 4 (2005): 355–68. http://dx.doi.org/10.1017/s0016756805000841.

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We describe the stratigraphical/sedimentological and structural evolution of the Manyara Rift in the Tanzania Divergence Zone, East Africa. The rift-related Manyara Beds on the shoaling side of the Manyara Rift were deposited between <1.7 and 0.4 Ma and can be separated into a lacustrine lower member and a fluvial upper member. The transition from lacustrine to fluvial sedimentation at ∼ 0.7 Ma appears to be related to a southward shift of major rift faulting. Fault geometry and the kinematics of the faults are consistent with major faulting during NE/E-directed extension. There is also evi
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22

ELS, B. G. "Anomalous pebble size variation in an erosive, Late Archaean braided stream: the Middelvlei gold placer, Witwatersrand, South Africa." Sedimentology 40, no. 1 (1993): 41–52. http://dx.doi.org/10.1111/j.1365-3091.1993.tb01089.x.

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23

BARRETT, T. J., and P. W. FRALICK. "Turbidites and iron formations, Beardmore-Geraldton, Ontario: application of a combined ramp/fan model to Archaean clastic and chemical sedimentation." Sedimentology 36, no. 2 (1989): 221–34. http://dx.doi.org/10.1111/j.1365-3091.1989.tb00604.x.

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24

England, Gavin L., Birger Rasmussen, Bryan Krapez, and David I. Groves. "Palaeoenvironmental significance of rounded pyrite in siliciclastic sequences of the Late Archaean Witwatersrand Basin: oxygen-deficient atmosphere or hydrothermal alteration?" Sedimentology 49, no. 6 (2002): 1133–56. http://dx.doi.org/10.1046/j.1365-3091.2002.00479.x.

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25

Corcoran, P. L., W. U. Mueller, and E. H. Chown. "Climatic and tectonic influences on fan deltas and wave- to tide-controlled shoreface deposits: evidence from the Archaean Keskarrah Formation, Slave Province, Canada." Sedimentary Geology 120, no. 1-4 (1998): 125–52. http://dx.doi.org/10.1016/s0037-0738(98)00030-x.

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26

Thomson, B. "Petrology and stratigraphy of some texturally well preserved thin komatiites from Kambalda, Western Australia." Geological Magazine 126, no. 3 (1989): 249–61. http://dx.doi.org/10.1017/s0016756800022342.

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AbstractArchaean komatiite volcanics at Kambalda, Western Australia have been metamorphosed to upper greenschist–lower amphibolite grade and have experienced intense though heterogeneously developed polyphase deformation. Despite this, preservation of igneous textural features is often good, particularly in areas which underwent only ‘static style’ metamorphism. Thin lavas from the Tripod Hill Member of the Kambalda Komatiite Formation over the western margin of the Hunt nickel shoot display textural elements and facies variations which are virtually identical to those found in fresher thin ko
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27

Wilson, Allan H., and J. Adrian Versfeld. "The early Archaean Nondweni greenstone belt, southern Kaapvaal Craton, South Africa, Part I. Stratigraphy, sedimentology, mineralization and depositional environment." Precambrian Research 67, no. 3-4 (1994): 243–76. http://dx.doi.org/10.1016/0301-9268(94)90012-4.

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28

CHADWICK, BRIAN. "The stratigraphy of a sheet of supracrustal rocks within high-grade orthogneisses and its bearing on Late Archaean structure in southern West Greenland." Journal of the Geological Society 147, no. 4 (1990): 639–52. http://dx.doi.org/10.1144/gsjgs.147.4.0639.

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29

Barnhart, Elliott P., Kara Bowen De León, Bradley D. Ramsay, Alfred B. Cunningham, and Matthew W. Fields. "Investigation of coal-associated bacterial and archaeal populations from a diffusive microbial sampler (DMS)." International Journal of Coal Geology 115 (August 2013): 64–70. http://dx.doi.org/10.1016/j.coal.2013.03.006.

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30

Brooks, Kent. "The young Earth and the story of the early Archaean rocks of West Greenland." Geology Today 27, no. 1 (2011): 15–19. http://dx.doi.org/10.1111/j.1365-2451.2011.00778.x.

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31

Lin, Genmei, Jianguo Lu, Kunwen Luo, et al. "Characterization of bacterial and archaeal community structure in deep subsurface sediments in the Shenhu area, northern South China Sea." Marine and Petroleum Geology 136 (February 2022): 105468. http://dx.doi.org/10.1016/j.marpetgeo.2021.105468.

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32

Gardiner, N. J., J. A. Mulder, C. L. Kirkland, T. E. Johnson, and O. Nebel. "Palaeoarchaean TTGs of the Pilbara and Kaapvaal cratons compared; an early Vaalbara supercraton evaluated." South African Journal of Geology 124, no. 1 (2021): 37–52. http://dx.doi.org/10.25131/sajg.124.0010.

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Abstract The continental crust that dominates Earth’s oldest cratons comprises Eoarchaean to Palaeoarchaean (4.0 to 3.2 Ga) felsic intrusive rocks of the tonalite-trondhjemite-granodiorite (TTG) series. These are found either within high-grade gneiss terranes, which represent Archaean mid-continental crust, or low-grade granite-greenstone belts, which represent relic Archaean upper continental crust. The Palaeoarchaean East Pilbara Terrane (EPT), Pilbara Craton, Western Australia, and the Barberton Granite-Greenstone Belt (BGGB), Kaapvaal Craton, southern Africa, are two of the best exposed gr
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33

Aucelli, Pietro, Vincenzo Amato, Massimo Cesarano, et al. "New morphostratigraphic and chronological constraints for the Quaternary paleosurfaces of the Molise Apennine (southern Italy)." Geologica Carpathica 62, no. 1 (2011): 17–26. http://dx.doi.org/10.2478/v10096-011-0002-2.

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New morphostratigraphic and chronological constraints for the Quaternary paleosurfaces of the Molise Apennine (southern Italy)The Molise Apennines feature numerous relicts of paleosurfaces, mostly of erosional origin, which represent the remnants of gently-rolling ancient landscapes now hanging at different altitudes above the local base-levels of erosion. Their genesis can be related to prolonged periods of relative tectonic stability alternating with periods of uplift, or to the interplay between steady tectonic uplift and climatic fluctuations. Four orders of paleosurfaces were recognized:
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34

Bruins, Hendrik J., Johannes van der Plicht, and J. Alexander MacGillivray. "The Minoan Santorini Eruption and Tsunami Deposits in Palaikastro (Crete): Dating by Geology, Archaeology, 14C, and Egyptian Chronology." Radiocarbon 51, no. 2 (2009): 397–411. http://dx.doi.org/10.1017/s003382220005579x.

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Deposits from the Minoan Santorini (Thera) eruption in the eastern Mediterranean region constitute the most important regional stratigraphic marker in the chronological perplexity of the 2nd millennium BCE. Extensive tsunami deposits were discovered in Crete at the Minoan archaeological site of Palaikastro, containing reworked volcanic Santorini ash. Hence, airborne deposition of volcanic ash, probably during the 1st (Plinian) eruption phase, preceded the tsunami, which was apparently generated during the 3rd or 4th phase of the eruption, based on evidence from Thera. Average radiocarbon dates
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35

Chen, Duo Fu, Yong Yang Huang, Xun Lai Yuan, and Lawrence M. Cathles. "Seep carbonates and preserved methane oxidizing archaea and sulfate reducing bacteria fossils suggest recent gas venting on the seafloor in the Northeastern South China Sea." Marine and Petroleum Geology 22, no. 5 (2005): 613–21. http://dx.doi.org/10.1016/j.marpetgeo.2005.05.002.

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36

Lysenko, V. I., S. A. Sadykov, and T. V. Mikhailichenko. "Hydrothermal-bacterial structures with a brachiopod fauna on the surface of Tessel paleovolcano (South coast of Crimea)." LITHOSPHERE (Russia) 22, no. 4 (2022): 497–511. http://dx.doi.org/10.24930/1681-9004-2022-22-4-497-511.

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Research subject. For the first time, the results of a study of hydrothermal-bacterial carbonate structures and a shell bank of brachiopods on the surface of the effusive sequence of the Late Triassic Tessel paleovolcano are presented. Methods. Petrographic thin sections were studied using an Olympus BX 5 microscope with an Olympus DP 12 camera. Geochemical investigations were performed according to the conventional methodology by an inductively coupled plasma mass spectrometer (ICP-MS). The isotopic composition of carbon was determined by isotope ratio mass spectrometry (IRMS) by a Deltaplus
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37

García Martínez, Daniel, Mathieu Duval, Jianxin Zhao, et al. "Los Villares locality (Ruidera, Castilla-La Mancha, Spain): a new Middle Pleistocene fossil assemblage from the Southern Iberian Plateau with possible evidence of human activity." Cuaternario y Geomorfología 36, no. 1-2 (2022): 7–35. http://dx.doi.org/10.17735/cyg.v36i1-2.90422.

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We present the discovery of a Middle Pleistocene fossil assemblage at Los Villares (Ruidera, Ciudad Real, Castilla-La Mancha), which has possible evidence of associated human activity. The potential of the site has been evaluated through multidisciplinary research including taxonomy, anatomy, deep learning, and direct dating of fossil remains. A surface study carried out in 2017, over a very limited area (2 m2) on the slope of one of the Ruidera lakes led to the discovery of more than 50 fossil specimens, including cranial (mainly teeth) and postcranial remains. This rich assemblage is dominat
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Usoltseva, Olga, and Elena Kozlovskaya. "Studying local earthquakes in the area Baltic-Bothnia Megashear using the data of the POLENET/LAPNET temporary array." Solid Earth 7, no. 4 (2016): 1095–108. http://dx.doi.org/10.5194/se-7-1095-2016.

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Abstract. Earthquakes in areas within continental plates are still not completely understood, and progress on understanding intraplate seismicity is slow due to a short history of instrumental seismology and sparse regional seismic networks in seismically non-active areas. However, knowledge about position and depth of seismogenic structures in such areas is necessary in order to estimate seismic hazard for such critical facilities such as nuclear power plants and nuclear waste deposits. In the present paper we address the problem of seismicity in the intraplate area of northern Fennoscandia u
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"Chapter 1 Introduction." Geological Society, London, Memoirs 26, no. 1 (2002): 1–10. http://dx.doi.org/10.1144/gsl.mem.2002.026.01.01.

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The Lewisian outcrops at Gairloch and Loch Maree have long been regarded as key areas in the Lewisian complex of NW Scotland because of the presence of the supracrustal rocks of the Palaeoproterozoic Loch Maree Group enclosed within the Archaean gneisses. Long before the age of this Group was known, attention was focused on these areas because the existence of metasedimentary rocks offered the possibility of establishing a stratigraphy within the Lewisian complex. Until relatively recently, Lewisian 'stratigraphy' was based entirely on the relative ages of igneous and metamorphic events.The ea
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40

Henriksen, Niels, A. K. Higgins, Feiko Kalsbeek, and T. Christopher R. Pulvertaft. "Greenland from Archaean to Quaternary. Descriptive text to the Geological map of Greenland, 1:2 500 000." GEUS Bulletin, December 29, 2000, 2–93. http://dx.doi.org/10.34194/ggub.v185.5197.

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NOTE: This monograph was published in a former series of GEUS Bulletin. Please use the original series name when citing this monograph, for example:
 Henriksen, N., Higgins, A., Kalsbeek, F., & Pulvertaft, T. C. R. (2000). Greenland from Archaean to Quaternary. Descriptive text to the Geological map of Greenland, 1:2 500 000. Geology of Greenland Survey Bulletin, 185, 2-93. https://doi.org/10.34194/ggub.v185.5197
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 The geological development of Greenland spans a period of nearly 4 Ga, from the earliest Archaean to the Quaternary. Greenland is the largest isla
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Garde, Adam A. "Accretion and evolution of an Archaean high-grade grey gneiss – amphibolite complex: the Fiskefjord area, southern West Greenland." GEUS Bulletin, October 10, 1997, 1–115. http://dx.doi.org/10.34194/ggub.v179.5075.

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NOTE: This monograph was published in a former series of GEUS Bulletin. Please use the original series name when citing this series, for example:
 Garde, A. A. 1997: Accretion and evolution of an Archaean high-grade grey gneiss – amphibolite complex: the Fiskefjord area, southern West Greenland. Geology of Greenland Survey Bulletin 177, 115 pp.
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 The Fiskefjord area in southern West Greenland, part of the Akia tectono-stratigraphic terrane, comprises a supracrustal association and two groups of grey quartzo-feldspathic orthogneises c. 3200 and 3000 Ma old. The su
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42

Rasmussen, Henrik, and Lars Frimodt Pedersen. "Stratigraphy, structure and geochemistry of Archaean supracrustal rocks from Oqaatsut and Naajaat Qaqqaat, north-east Disko Bugt, West Greenland." GEUS Bulletin, July 22, 1999, 65–78. http://dx.doi.org/10.34194/ggub.v181.5114.

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NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example:
 Rasmussen, H., & Frimodt Pedersen, L. (1999). Stratigraphy, structure and geochemistry of Archaean supracrustal rocks from Oqaatsut and Naajaat Qaqqaat, north-east Disko Bugt, West Greenland. Geology of Greenland Survey Bulletin, 181, 65-78. https://doi.org/10.34194/ggub.v181.5114
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 Two Archaean supracrustal sequences in the area north-east of Disko Bugt, c. 1950 and c. 800 m in thickness, are dominated by pelitic a
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Runge, Eric A., Jan‐Peter Duda, Martin J. Van Kranendonk, and Joachim Reitner. "Earth’s oldest tsunami deposit? Early Archaean high‐energy sediments in the ca 3.48 Ga Dresser Formation (Pilbara, Western Australia)." Depositional Record, February 2022. http://dx.doi.org/10.1002/dep2.175.

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