Titlebook: Himalayan Thick-Skin Basement Deformation of the Ladakh Batholith, Leh-Ladakh Region, NW India; Michael George Petterson Book 2023 The Edi

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Overview of the Geology, Structure, and Tectonics of the Ladakh Batholith and Indus Suture Rocks,rop 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, c

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,Structure and Lithology of the Indus Suture Rocks (,) in the Leh–Ladakh Region,ell exposed, forming cliffs and mountains with a c. 2000 m + vertical relief in places. The unit is well bedded and contiguously bedded. Thrust and fault structures are clearly visible in mountainside outcrops. There is a wide variation in clastic lithological character from coarse conglomerates to

Spinous-Process

,Deformation Model for the Ladakh Batholith in the Leh–Ladakh Region, of magmatism. Crustal depth pluton emplacement estimates range between 7 and 15 km. Low temperature geochronological studies indicate the batholith was uplifted to c. 3 km between 8 and 30 Ma. Zanskar structural studies indicate active cover-basement thrusting between 45 and 25 Ma with cover deform

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Book 2023ks that predominantly moved towards the N-NE.  Whilst deformation within cover sequences influences the basement structures, and helps break up the basement into crustal blocks, there is a clear distinction in deformation between the basement and cover sequences. Basement batholith deformation is mo

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,Geo-tectonic and, Topographic, and Geographical Setting of the Leh–Ladakh Region: Study Scope and M km long and 6 km wide to the north of the study region. Geological fieldwork, mapping, and structural geological studies, together with photographic image, photo-mosaic, and satellite image anlaysis, are applied to the fundamental research question: ‘how has the Ladakh batholith/basement deformed d

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Overview of the Geology, Structure, and Tectonics of the Ladakh Batholith and Indus Suture Rocks, 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-li