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  2. Supracrustal rock - Wikipedia

    en.wikipedia.org/wiki/Supracrustal_rock

    Supracrustal rocks (supra (Latin for "above")) are rocks that were deposited on the existing basement rocks of the crust, hence the name. They may be further metamorphosed from both sedimentary and volcanic rocks .

  3. Eoarchean geology - Wikipedia

    en.wikipedia.org/wiki/Eoarchean_geology

    Eoarchean geology is the study of the oldest preserved crustal fragments of Earth during the Eoarchean era from 4.031 to 3.6 billion years ago. Major well-preserved rock units dated to this era are known from three localities, the Isua Greenstone Belt in Southwest Greenland, the Acasta Gneiss in the Slave Craton in Canada, and the Nuvvuagittuq Greenstone Belt in the eastern coast of Hudson Bay ...

  4. Isua Greenstone Belt - Wikipedia

    en.wikipedia.org/wiki/Isua_Greenstone_Belt

    The Isua Greenstone Belt is an Archean greenstone belt in southwestern Greenland, aged between 3.7 and 3.8 billion years. [2] The belt contains variably metamorphosed mafic volcanic and sedimentary rocks, and is the largest exposure of Eoarchaean supracrustal rocks on Earth. [3]

  5. Dharwar Craton - Wikipedia

    en.wikipedia.org/wiki/Dharwar_Craton

    The location map of the Dharwar Craton. The shaded area represents the Dharwar Craton. Generated from GeoMapApp (Ryan et al., 2009). [1]The Dharwar Craton is an Archean continental crust craton formed between 3.6-2.5 billion years ago (), which is located in southern India and considered the oldest part of the Indian peninsula.

  6. Lewisian complex - Wikipedia

    en.wikipedia.org/wiki/Lewisian_complex

    These rocks are of Archaean and Paleoproterozoic age, ranging from 3.0–1.7 billion years . They form the basement on which the Stoer Group, Wester Ross Supergroup and probably the Loch Ness Supergroup sediments were deposited. The Lewisian consists mainly of granitic gneisses with a minor amount of supracrustal rocks.

  7. Peninsular Gneiss - Wikipedia

    en.wikipedia.org/wiki/Peninsular_Gneiss

    The supracrustal rocks of the Dharwar Group of the southern Indian Peninsula, as depicted in the geological map of South India, have the Peninsular Gneiss as the basement rock formation, also stated to be the remobilized basement.

  8. Geology of Zimbabwe - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Zimbabwe

    The oldest supracrustal rocks are the Sebakwian Group (3.5 Ga) exposed around Shurugwi and Mashava, and northwest of Gweru, within the central craton. This group consist of metavolcanic rocks, including komatiite and basalt, banded iron formation, and clastic metasedimentary rocks. The Sebakwian Group is succeeded by the Bulawayan Group ...

  9. Category:Sedimentary rocks - Wikipedia

    en.wikipedia.org/wiki/Category:Sedimentary_rocks

    Pages in category "Sedimentary rocks" The following 136 pages are in this category, out of 136 total. ... Supracrustal rock; Sylvinite; Syneresis crack; T. Taconite;