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- W2382430069 abstract "Shihelagou lies to the south of the Yellow River near the Hetao area (the top of the Great Bend of the Yellow River in the Inner Mongolia). Shihelagou thrust nappe thrusting from north to south is recently discovered in the northern margin uplift belt of Ordos block during lately 1:250 000 regional geological survey in Baotou region. Hanging wall of the thrust is composed of the Palaeoproterozoic lowgrade quartzite, biotite granulitite and marble from basement. It's over to the Taiyuan Formation of Middle Carboniferous and Ermaying Formation of Middle Triassic. According to field geological relationship, the thrusting occurred in Late Jurassic and was coinstantaneous with late thrusting of Daqingshan thrust in the northern margin of Hetao Cenozoic fault basin, but their thrusting direction was reversal each other in result forming late Jurassic fanshaped thrusts in the center of present Hetao Cenozoic fault basin. The discovery of Shihelagou thrust nappe is very important significance for discussing Mesozoic crust deformation characteristics of northern margin of North China and the character and formation process of the basement of Hetao Cenozoic fault basin." @default.
- W2382430069 created "2016-06-24" @default.
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- W2382430069 date "2004-01-01" @default.
- W2382430069 modified "2023-09-22" @default.
- W2382430069 title "Discovery of Shihelagou Thrust Nappe andIts Geological Significance" @default.
- W2382430069 hasPublicationYear "2004" @default.
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