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India-Asia collision was at 24°N and 50 Ma: palaeomagnetic proof from southernmost Asia
How and when India collided with Asia is crucial for global climate and continental dynamics. We present new palaeomagnetic data showing that the Xigaze forearc basin of southern Tibet was located at 24.2±5.9°N during 54–57 Ma, providing a direct constraint on the position of the southernmost margin...
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| 主要な著者: | , , , , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group
2012
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3514643/ https://ncbi.nlm.nih.gov/pubmed/23226592 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep00925 |
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