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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Damara Orogeny ： ウィキペディア英語版 Damara Orogeny The Damara Orogeny created the Naukluft Mountains between 550 Ma and 495 Ma.〔http://gondwanaresearch.com/gray.pdf〕〔JUNG, S. & MEZGER, K. 2003. U-Pb garnet chronometry in high-grade rocks; case studies from garnet ages and the role of high U-Th inclusions. Contributions to Mineralogy Petrology 146, 382-396.〕〔JUNG, S, HOERNES, S. & MEZGER, K. 2000. Geochronology and petrogenesis of Pan-African syn-tectonic S-type and post-tectonic A-type granite (Namibia) – products of melting of crustal sources, fractional crystallization and wall rock entrainment. Lithos 50, 259-287.〕〔KUKLA, C. 1993. Strontium isotope heterogeneities in amphibolite facies, banded metasediments— a case study from the Late Proterozoic Kuiseb Formation of the southern Damara Orogen, Central Namibia. Communications of the Geological Survey of Namibia Memoir 15, 139pp.〕〔KUKLA, C., KRAMM, U., KUKLA, P.A., OKRUSCH, M. 1991. U-Pb monazite data relating to metamorphism and granite intrusion in the northwestern Khomas Trough, Damara Orogen, Central Namibia. Communications of the Geological Survey of Namibia 7, 49-54.〕 The Damara Orogeny occurred late in the creation of Gondwana, at the intersection of the Congo craton and the Kalahari Craton.〔〔〔〔〔 == See also == * Supercontinent 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Damara Orogeny」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.