Subsidence history of the north Indian continental margin, Zanskar-Ladakh Himalaya, NW India
Detailed geological field mapping has allowed the restoration of two full stratigraphic sections through the highly deformed Mesozoic and Early Tertiary fold and thrust belt of the north Indian continental margin. The two sections, which are representative of a proximal and a distal facies on the ma...
المؤلفون الرئيسيون: | Corfield, R, Watts, A, Searle, M |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
2005
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مواد مشابهة
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Discussion on subsidence history of the north Indian continental margin, Zanskar-Ladakh Himalaya, NW India
حسب: Garzanti, E, وآخرون
منشور في: (2005) -
Structure of the North Indian continental margin in the Ladakh-Zanskar Himalayas: Implications for the timing of obduction of the Spontang ophiolite, India-Asia collision and deformation events in the Himalaya
حسب: Searle, M, وآخرون
منشور في: (1997) -
Crustal shortening estimates across the north Indian continental margin, Ladakh, NW India
حسب: Corfield, R, وآخرون
منشور في: (2000) -
Tectonic setting, origin, and obduction history of the spontang ophiolite, Ladakh Himalaya, NW India
حسب: Corfield, R, وآخرون
منشور في: (2001) -
Ladakh and Zanskar
حسب: Zgorzelski Marek
منشور في: (2006-12-01)