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• W4379032168 abstract "The Kohistan–Ladakh batholith forms the most voluminous geological unit within the Kohistan–Ladakh island arc terrane, constituting c. 80% of the outcrop area in the Ladakh region. The batholith is up to 30 km thick, with emplacement depth estimates of various components of the batholith ranging between 10 and < 2 kb (c. 35–7 km depth): in Ladakh estimates are > 4 to c. 2 kb (c. 15–7 km depth). The Ladakh batholith is heterogeneous and complex, comprising plutons, stocks, dykes and sills that range in composition from hornblende cumulates to felsic rich leucogranites. The proportion of lithological compositions exposed in the batholith is c. 10–20% mafic/ultramafic, 20–30% intermediate, 50% acid, and 10% leucocratic-felsic acid sheets. Primary mineralogy is dominated by hbl-biot-plag-qz-alk feld-with minor px. Minor mineralogy comprises zirc-sph-ilm-mag-py-cp-xen. Batholith age estimates vary between 150 and < 30 Ma, although mostly 120 Ma or less, and 78–45 Ma in the Leh-Ladakh region. Metamorphic grade varies from very low to amphibolite grade, with sericite-lower greenschist grade being most common. Non-batholithic rocks in Ladakh comprise the Late Triassic–Cretaceous clastic-limestone marine Lamayuru Complex, the Jurassic–Cretaceous Dras Volcanics, the Palaeocene–Eocene marine-sedimentary Tar Formation, including the youngest marine Nummulitic limestone, and the Eocene-Upper Miocene Indus Suture molasse sequence. Deformation has produced central upright, southerly south-verging, and northerly north-verging thrusts and folds, with deformation from c. 70 Ma to the Pliocene, and modern active tectonics. Low temperature geothermometry suggests Ladakh uplifted through the 150 °C isotherm between 30 and 8 Ma (youngest ages in north Ladakh)." @default.
• W4379032168 created "2023-06-02" @default.
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• W4379032168 date "2023-01-01" @default.
• W4379032168 modified "2023-09-24" @default.
• W4379032168 title "Overview of the Geology, Structure, and Tectonics of the Ladakh Batholith and Indus Suture Rocks" @default.
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• W4379032168 doi "https://doi.org/10.1007/978-3-031-31566-4_2" @default.
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