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The crustal shortening /thickening within high Tibet and its tectonic ...

The crustal shortening /thickening within high Tibet and its tectonic ...

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<strong>Tibet</strong>an Plateau : Tectonic Setting<br />

1) India <strong>and</strong> Asia collide each other along<br />

Himalayas at 40-60 Ma<br />

2) Since then, India, subcontinent is moving<br />

northward at 40-55 mm/a<br />

3) <strong>Tibet</strong> is deforming in the Cenozoic era ,<br />

associated with various styles of <strong>tectonic</strong><br />

features in continent<br />

faulting, metamorphism, sedimentation,<br />

magmatism, earthquake, so on<br />

As summaried by Molnar & Tapponnier,<br />

Science,189, 419, 1975<br />

Features of recent continental <strong>tectonic</strong>s in Asia<br />

can be interpreted as results of the India-<br />

Eurasia collision.<br />

.<br />

Tapponnier et al., Science ,<br />

294,1671, 2001

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