Pliocene and Quaternary environmental change in Kashmir, north-west Himalaya
<p>Late Cainozoic environmental changes in Kashmir (33°30' to 34°30' N: 74°10' to 75°30' E) have been reconstructed using a range of techniques. The sedimentary record in Kashmir consists of a thick (>1000m) basin-fill sequence known as the Karewa group, together wi...
| المؤلفون الرئيسيون: | , |
|---|---|
| التنسيق: | أطروحة |
| اللغة: | English |
| منشور في: |
1989
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| الموضوعات: |