Journal
GEOLOGY
Volume 38, Issue 9, Pages 807-810Publisher
GEOLOGICAL SOC AMER, INC
DOI: 10.1130/G31087.1
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Funding
- Natural Environment Research Council [NE/B503192/1]
- Natural Environment Research Council [ceh010010, NE/B503192/1] Funding Source: researchfish
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A combination of sediment petrography, detrital zircon U-Pb, and fission-track dating is used to show that provenance of the Paleogene sedimentary rocks exposed in the Makran region of southern Iran and the Katawaz basin of Pakistan is consistent with a source from the nascent western Himalaya and associated magmatic arc. Results from this important archive show that Paleogene erosion was focused mainly on the arc and northern Indian margin, and, in contrast to the east-central Himalaya, we have not detected widespread rapid exhumation indicative of strong forcing by climate-driven erosion at that time.
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