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

Quartz and calcite veins are omnipresent in the Indus basin sedimentary rocks (IBSRs) of the Indus Tsangpo suture zone (ITSZ) which were formed by the accumulation of sediments derived from both sides of the tectonic plate. These veins appear to have formed just after the sediment diagenesis and wer...

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Veröffentlicht in:	Journal of Earth System Science 2019-07, Vol.128 (5), p.138, Article 138
Hauptverfasser:	Kharya, Aditya, Sachan, Himanshu K, Santosh, M, Singh, Sunil K, Tiwari, Sameer K
Format:	Artikel
Sprache:	eng
Schlagworte:	Calcite Diagenesis Earth Earth and Environmental Science Earth mantle Earth Sciences Fingerprinting Fluids Forearc basins Geochemistry Geology Isotopes Metamorphism Orogeny Oxygen Plate tectonics Plates (tectonics) Quartz Rare earth elements Seawater Sediment Sedimentary rocks Sedimentation Sediments Space Exploration and Astronautics Space Sciences (including Extraterrestrial Physics Strontium Strontium isotopes Systematics Veins Veins (geology)
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