Although motion is likely to have varied more smoothly than these results would allow, the geological record also suggests a sequence of distinct episodes, at about the same times. Hence we suggest that no single event should be regarded as the collision of India with Asia. The deceleration of...
印度-亚洲大陆主碰撞过程的火山作用响应 response of volcanism to the india-asia collision 星级: 14 页 印度-亚洲大陆碰撞-后碰撞过程的火山作用记录 星级: 1页 印度-亚洲碰撞大地构造 on the tectonics of the india-asia collision 下载积分:2000 内容提示: 爹;51芎≯11曹地质学报ACTA G EO LO G I CAS...
Ultrahigh-pressure (UHP) rocks in the NW Himalaya are some of the youngest on Earth, and allow testing of critical questions of UHP formation and exhumation and the timing of the India–Asia collision. Initial collision of India with Asia is widely cited as being at 55 ± 1 ...
India-Eur-asia collision.The samples of muscovite and biotite mylonitic rock were collected from the different parts of deformation in the shear zone to analyze the chronology with the mica 40Ar-39Ar dating.The tested ages including 53.39±0.57 Ma, 39.45±0.42 Ma and 29.41±0.32 Ma in three ...
of the continental collision. Integrated with tectonic deformation, foreland basins, provenance analysis and paleomagnetism, an alternative model was first proposed suggesting that the collision between India and Asia first occurred in the central section of the YTSZ between ca. 65 Ma and 63 Ma, ...
of south and east Asia to Siberia, culminating in the collision of India with Asia during the Cenozoic. Palaeomagnetic data have already demonstrated that the Kolyma and Sikhote Alin blocks of eastern Asia collided with the main continent along the late Mesozoic fold belts of Verkhoyansk and ...
and left-lateral kinematic indicators. U–Pb radiometric ages of∼23 Myr imply that strike-slip movement along this shear zone occurred in the Oligo-Miocene. The strain observed suggests that collision of India with Asia displaced Indochina at least 500km southeastwards relative to South China....
Abstract The eastern Himalayan syntaxis in Namjagbarwa is a high-grade metamorphic terrain formed by the India-Eurasia collision and northward indentation of the Indian continent into Asia. Right- and left-lateral slip zones were formed by the indentation on the eastern and western boundaries ...
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Convergence between the Indian and Asian plates has reshaped large parts of Asia, changing regional climate and biodiversity, yet geodynamic models fundamentally diverge on how convergence was accommodated since the India–Asia collision. Here we report palaeomagnetic data from the Burma Terrane, which...