Isotopic fingerprinting of fluid circulation at the terminal stage of the Himalayan orogeny: An example from the Himalayan forearc basin, Indus Tsangpo suture zone, Ladakh, India.

MLA

Kharya, Aditya, et al. “Isotopic Fingerprinting of Fluid Circulation at the Terminal Stage of the Himalayan Orogeny: An Example from the Himalayan Forearc Basin, Indus Tsangpo Suture Zone, Ladakh, India.” Journal of Earth System Science, vol. 128, no. 5, July 2019, p. N.PAG. EBSCOhost, https://doi.org/10.1007/s12040-019-1139-0.

APA

Kharya, A., Sachan, H. K., Santosh, M., Singh, S. K., & Tiwari, S. K. (2019). Isotopic fingerprinting of fluid circulation at the terminal stage of the Himalayan orogeny: An example from the Himalayan forearc basin, Indus Tsangpo suture zone, Ladakh, India. Journal of Earth System Science, 128(5), N.PAG. https://doi.org/10.1007/s12040-019-1139-0

Chicago

Kharya, Aditya, Himanshu K Sachan, M Santosh, Sunil K Singh, and Sameer K Tiwari. 2019. “Isotopic Fingerprinting of Fluid Circulation at the Terminal Stage of the Himalayan Orogeny: An Example from the Himalayan Forearc Basin, Indus Tsangpo Suture Zone, Ladakh, India.” Journal of Earth System Science 128 (5): N.PAG. doi:10.1007/s12040-019-1139-0.