Origin of Indus ophiolite-hosted ophicarbonate veins: Isotopic evidence of mixing between seawater and continental crust-derived fluid during Neo-Tethys closure
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Das, S., Basu, A. R., Mukherjee, B. K., Marcantonio, F., Sen, K., Bhattacharya, S., & Gregory, R. T.
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Das, Souvik||Basu, Asish R||Mukherjee, Barun K||Marcantonio, Franco||Sen, Koushick||Bhattacharya, Satadru||Gregory, Robert T
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Continental Crust-derived Fluid
Fischer-tropsch Reaction
Himalaya
Ophicarbonate
Seawater
Srisotope
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http://dx.doi.org/10.1016/j.chemgeo.2020.119772