Indian Ocean Plate Reconstructions Since the Late Jurassic

التفاصيل البيبلوغرافية
العنوان: Indian Ocean Plate Reconstructions Since the Late Jurassic
المؤلفون: Royer, JY, Sclater, JG, Sandwell, DT, Cande, SC, Schlich, R, Munschy, M, Dyment, J, Fisher, RL, Mueller, RD, Coffin, MF, Patriat, P, Bergh, HW
بيانات النشر: American Geophysical Union
سنة النشر: 1992
مصطلحات موضوعية: Earth Sciences, Geology, Marine Geoscience, geo
الوصف: The evolution of the Indian Ocean (Figure 1) since the Late Jurassic can be summarized in three main periods of seafloor spreading separated by two major plate boundary reorganizations [Royer, 1992]. From breakup of Gondwana at about 160 Ma (Figure 2) to the Late Cretaceous (-90/95 Ma), the opening of the Indian Ocean coincided with divergence of two superblocks, Africa-South America and Madagascar-Seychelles-India-Australia-Antarctica, which further fragmented in the Early Cretaceous (chron M0; Figure 3) into Africa-Madagascar-India and Australia-Antarctica. This two-plate system broke into a five-plate system during the Late Cretaceous with seafloor spreading between Madagascar and India-Seychelles and between Australia and Antarctica (Figures 4 to 8). The second major plate boundary reorganization occurred during the middle Eocene and coincided with the collision of India with Eurasia (Figures 8 and 9). The resulting plate boundary system has prevailed until present (Figures 8 to 12, and 1). The final events of this last phase were opening of the Gulf of Aden at about Chron 5 (10 Ma) and onset of the intraplate deformation in the Central Indian Basin between India and Australia (7 Ma). Evolution of the plate geometry is summarized in Figure 13.
نوع الوثيقة: book part
اللغة: English
العلاقة: http://ecite.utas.edu.au/73788/1/Royer_et_al_AGU70_1992.pdfTest; https://doi.org/10.1029/GM070p0471Test
DOI: 10.1029/GM070p0471
الإتاحة: https://doi.org/10.1029/GM070p0471Test
http://ecite.utas.edu.au/73788/1/Royer_et_al_AGU70_1992.pdfTest
حقوق: undefined
رقم الانضمام: edsbas.E898795B
قاعدة البيانات: BASE