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Paleocene latitude of the Kohistan–Ladakh arc indicates multistage India–Eurasia collision

We report paleomagnetic data showing that an intraoceanic Trans-Tethyan subduction zone existed south of the Eurasian continent and north of the Indian subcontinent until at least Paleocene time. This system was active between 66 and 62 Ma at a paleolatitude of 8.1 ± 5.6 °N, placing it 600–2,300 km...

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Vydáno v:Proc Natl Acad Sci U S A
Hlavní autoři: Martin, Craig R., Jagoutz, Oliver, Upadhyay, Rajeev, Royden, Leigh H., Eddy, Michael P., Bailey, Elizabeth, Nichols, Claire I. O., Weiss, Benjamin P.
Médium: Artigo
Jazyk:Inglês
Vydáno: National Academy of Sciences 2020
Témata:
On-line přístup:https://ncbi.nlm.nih.gov/pmc/articles/PMC7703637/
https://ncbi.nlm.nih.gov/pubmed/33148806
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2009039117
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