Abstract
Neodymium (Nd) isotopes from the Himalayan fold-thrust belt and its associated foreland basin deposits are useful for distinguishing between Himalayan tectonostratigraphic zones and revealing the erosional unroofing history as controlled by the kinematic development of the orogen. Neodymium isotopic data from the Himalayan fold-thrust belt in Nepal ( n=35) reveal that the Lesser Himalayan zone consistently has a more negative ϵ Nd(0) value than the Greater and Tibetan Himalayan zones. Our data show the average ϵ Nd(0) value in the Lesser Himalayan zone is −21.5, whereas the Greater and Tibetan Himalayan zones have an average ϵ Nd(0) value of −16. These consistently distinct values throughout Nepal enable the use of Nd isotopes as a technique for distinguishing between Lesser Himalayan zone and Greater Himalayan zone rock. The less negative ϵ Nd(0) values of the Greater Himalayan rocks support the idea that the Greater Himalayan zone is not Indian basement, but rather a terrane that accreted onto India during Early Paleozoic time. Neodymium isotopic data from Eocene through Pliocene foreland basin deposits ( n=34) show that sediment provenance has been dominated by Greater and Tibetan Himalayan detritus across Nepal. The ϵ Nd( T) values in the synorogenic rocks in western and central Nepal generally show an up-section shift toward more negative values and record the progressive unroofing of the different tectonostratigraphic zones. At ∼10 Ma in Khutia Khola and ∼11 Ma in Surai Khola, a shift in ϵ Nd( T) values from −16 to −18 marks the erosional breaching of a large duplex in the northern part of the Lesser Himalayan zone. This shift is not seen in eastern Nepal, where the ϵ Nd( T) values remain close to −16 throughout Miocene time because there has been less erosional unroofing in this region.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
