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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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11#
發(fā)表于 2025-3-23 09:42:09 | 只看該作者
12#
發(fā)表于 2025-3-23 14:29:27 | 只看該作者
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??4 to c. 2?kb (c. 15–7?km depth). The Ladakh batholith is heterogeneous and complex, c
13#
發(fā)表于 2025-3-23 21:44:57 | 只看該作者
14#
發(fā)表于 2025-3-24 01:04:58 | 只看該作者
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發(fā)表于 2025-3-24 06:21:06 | 只看該作者
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發(fā)表于 2025-3-24 08:17:33 | 只看該作者
,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
17#
發(fā)表于 2025-3-24 12:03:00 | 只看該作者
,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
18#
發(fā)表于 2025-3-24 18:00:39 | 只看該作者
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
19#
發(fā)表于 2025-3-24 19:47:56 | 只看該作者
,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
20#
發(fā)表于 2025-3-24 23:12:53 | 只看該作者
Overview of the Geology, Structure, and Tectonics of the Ladakh Batholith and Indus Suture Rocks, vary between 150 and?
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