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The restoration is time-calibrated with all available U\u2013Pb datings.<\/jats:p>\n          <jats:p>\n            Between incompletely preserved basin sequences, two superposed Palaeoarchaean volcano-sedimentary basins (the Coongan and Salgash Basins) are separated by an eastwards time-transgressive interface tentatively interpreted as an onlap surface. For over 140\u2005Ma, the basin margin architecture was structurally controlled by superposed extensional growth fault arrays (D\n            <jats:sub>1<\/jats:sub>\n            ) with associated dyke swarms in a curved pattern spatially not related to that of the actual distribution of granite domes and greenstone belts.\n          <\/jats:p>\n          <jats:p>\n            The basins are interpreted to have formed by collapse after arching above hotspots due to phase transitions by mini-subduction of slabs of cooled water-saturated basalt towards the base of an originally\n            <jats:italic>c.<\/jats:italic>\n            45\u2005km mafic crust. At\n            <jats:italic>c.<\/jats:italic>\n            3.31\u2005Ga, the extension was replaced by plate-driven regional NW\u2013SE compression (D\n            <jats:sub>2<\/jats:sub>\n            ) inferred from NW-over-SE shear and ramp-and-flat thrusts, partly reversing offsets of the D\n            <jats:sub>1<\/jats:sub>\n            extension. The recognition of widespread D\n            <jats:sub>2<\/jats:sub>\n            pre-doming compression is important because it triggered the\n            <jats:italic>c.<\/jats:italic>\n            3.18\u2005Ga start of formation of the dome-and-keel pattern (D\n            <jats:sub>3<\/jats:sub>\n            ) visible today, which culminated at\n            <jats:italic>c.<\/jats:italic>\n            2.9\u2005Ga.\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            Eight figures, numbered \u2018Supplementary material fig. a\u2013h\u2019, and a GPS list of observation sites are available at:\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.3808243\">https:\/\/doi.org\/10.6084\/m9.figshare.c.3808243<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2016-127","type":"journal-article","created":{"date-parts":[[2017,6,30]],"date-time":"2017-06-30T00:40:12Z","timestamp":1498783212000},"page":"1090-1112","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":30,"title":["Archaean basin margin geology and crustal evolution: an East Pilbara traverse"],"prefix":"10.1144","volume":"174","author":[{"given":"Wouter","family":"Nijman","sequence":"first","affiliation":[{"name":"Department of Earth Sciences, Faculty of Geosciences, Utrecht University, PO Box 80115, 3508 TC Utrecht, the Netherlands"}]},{"given":"Armelle","family":"Kloppenburg","sequence":"additional","affiliation":[{"name":"4DGeo Structural Geology, Daal en Bergselaan 80, 2565 AH The Hague, the Netherlands"}]},{"given":"Sjoukje T.","family":"de Vries","sequence":"additional","affiliation":[{"name":"Department of Earth Sciences, Faculty of Geosciences, Utrecht University, PO Box 80115, 3508 TC Utrecht, the Netherlands"}]}],"member":"1881","published-online":{"date-parts":[[2017,6,6]]},"reference":[{"key":"e_1_3_4_2_1","volume-title":"Structural Geology Algorithms: Vectors and Tensors","author":"Allmendinger R.W.","year":"2012","unstructured":"Allmendinger, R.W., Cardozo, N. & Fisher, D. 2012. 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