Relevant bibliographies by topics / Geology, Structural Kumaun Himalaya

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters

Academic literature on the topic 'Geology, Structural Kumaun Himalaya'

Author: Grafiati
Published: 11 December 2022
Last updated: 31 July 2025

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Journal articles on the topic "Geology, Structural Kumaun Himalaya"

1

Puniya, M. K., R. C. Patel, and P. D. Pant. "Structural and thermochronological studies of the Almora klippe, Kumaun, NW India: implications for crustal thickening and exhumation of the NW Himalaya." Geological Society, London, Special Publications 481, no. 1 (2018): 81–110. http://dx.doi.org/10.1144/sp481-2017-74.

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AbstractCrystalline klippen over the Lesser Himalayan Metasedimentary Sequence (LHMS) zone in the NW Himalaya have specific syn- and post-emplacement histories. These tectonics also provide a means to understand the driving factors responsible for the exhumation of the rocks of crystalline klippen during the Himalayan Orogeny. New meso- and microscale structural analyses, and thermochronological studies across the LHMS zone, Ramgarh Thrust (RT) sheet and Almora klippe in the eastern Kumaun region, NW Himalaya, indicate that the RT sheet and Almora klippe were a part of the Higher Himalayan Cry
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Mandal, Subhadip, Delores M. Robinson, Matthew J. Kohn, Subodha Khanal, and Oindrila Das. "Examining the tectono-stratigraphic architecture, structural geometry, and kinematic evolution of the Himalayan fold-thrust belt, Kumaun, northwest India." Lithosphere 11, no. 4 (2019): 414–35. http://dx.doi.org/10.1130/l1050.1.

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Abstract Existing structural models of the Himalayan fold-thrust belt in Kumaun, northwest India, are based on a tectono-stratigraphy that assigns different stratigraphy to the Ramgarh, Berinag, Askot, and Munsiari thrusts and treats the thrusts as separate structures. We reassess the tectono-stratigraphy of Kumaun, based on new and existing U-Pb zircon ages and whole-rock Nd isotopic values, and present a new structural model and deformation history through kinematic analysis using a balanced cross section. This study reveals that the rocks that currently crop out as the Ramgarh, Berinag, Ask
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Patel, R. C., Vikas Adlakha, Paramjeet Singh, Yogesh Kumar, and Nand Lal. "Geology, structural and exhumation history of the Higher Himalayan Crystallines in Kumaon Himalaya, India." Journal of the Geological Society of India 77, no. 1 (2011): 47–72. http://dx.doi.org/10.1007/s12594-011-0008-5.

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Chauhan, Dinesh S., Rajesh Sharma, and D. R. Rao. "A new occurrence of lazulite from the Main Central Thrust in Kumaun Himalaya, India: fluid inclusion, EPMA and Raman spectroscopy focusing on lazulite in a highly tectonized zone." Geological Society, London, Special Publications 481, no. 1 (2019): 211–30. http://dx.doi.org/10.1144/sp481-2018-117.

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AbstractThe present study reports and investigates ‘lazulite’ occurring in the vicinity of a highly tectonized zone of the Main Central Thrust (MCT) in the Himalaya. The azure blue lazulite, hosted in quartz veins, occurs in fractured Berinag quartzite, which forms the footwall of the MCT near Sobla village in NE Kumaun Himalaya, India. Lazulite was investigated using SEM-EDX, micro Raman spectroscopy, fluid inclusion microthermometry and electron probe microanalysis (EPMA). Lazulite contains inclusions of rutile and hematite and has Mg/(Mg+Fe) ratios of 0.86 to 0.90. The phosphorus in lazulit
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Patel, R. C., and Yogesh Kumar. "Late-to-post collisional brittle–ductile deformation in the Himalayan orogen: Evidences from structural studies in the Lesser Himalayan Crystallines, Kumaon Himalaya, India." Journal of Asian Earth Sciences 27, no. 5 (2006): 735–50. http://dx.doi.org/10.1016/j.jseaes.2005.06.010.

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6

Chamyal, L. S., and Manudip Kaur. "Structural set up in northern part of Kumaun Himalaya." Journal of Earth System Science 103, no. 1 (1994): 37–46. http://dx.doi.org/10.1007/bf02880807.

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7

Goel, O. P., S. S. Garhia, J. S. Mehta, and G. C. Kandpal. "An Interpretation of Regional Structures of Kumaun-Garhwal Himalaya Based on LANDSAT-I Imagery." Journal Geological Society of India 30, no. 4 (1987): 285–95. http://dx.doi.org/10.17491/jgsi/1987/300405.

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Abstract A preliminary study and interpretation of LANDSAT-I imagery, covering a large area of Kumaun-Garhwal Himalaya. lying between 79° - 80°30' East longitude and 29°0' - 30°30' North latitude, reveals the presence of four dominant directions of lineaments trending NS, NE-SW, NW/WN-SE/ESE and E-W. The lineament fabric of the region represents axial directions of major folds, regional strike trends of thrusts and of transverse or strike-slip faults. The study is supplemented by detailed structural analysis of mesoscopic folds, planar and linear features present in rocks of three sections of
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Rameshwar Rao, D., and Rajesh Sharma. "Petrogenesis of the granitoid rocks from Askot crystallines, Kumaun Himalaya." Journal of the Geological Society of India 74, no. 3 (2009): 363–74. http://dx.doi.org/10.1007/s12594-009-0133-6.

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S Parihar, D. "Physiography and Geology of Gori Ganga Watershed, Kumaun Higher Himalaya." International Journal of Science and Research (IJSR) 10, no. 2 (2021): 591–95. https://doi.org/10.21275/sr21212174338.

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10

Célérier, Julien, T. Mark Harrison, Andrew Alexander G. Webb, and An Yin. "The Kumaun and Garwhal Lesser Himalaya, India: Part 1. Structure and stratigraphy." Geological Society of America Bulletin 121, no. 9-10 (2009): 1262–80. http://dx.doi.org/10.1130/b26344.1.

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Dissertations / Theses on the topic "Geology, Structural Kumaun Himalaya"

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Celerier, Julien. "The structural and thermal evolution of the Kumaun and Garwhal [i.e. Garhwal] Lesser Himalaya, India." Phd thesis, 2007. http://hdl.handle.net/1885/149627.

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Aikman, Amos. "Tectonics of the eastern Tethyan Himalaya." Phd thesis, 2007. http://hdl.handle.net/1885/146541.

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Larson, Kyle. "The tectonometamorphic evolution of the Greater Himalayan sequence as exposed in central Nepal and adjacent south-central Tibet." Thesis, 2009. http://hdl.handle.net/1974/1737.

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Understanding the development of the Himalaya is critical to elucidating continental collisional processes. The Greater Himalayan sequence (GHS), the exhumed mid-crust of the Himalayan orogen, records the tectonometamorphic evolution of the Himalaya from its deep hinterland to its foreland. The GHS in central Nepal and adjacent Tibet is deformed pervasively; quartz c-axis orientation fabrics from across the GHS indicate that it was deformed at high temperatures (~550-650˚C). The asymmetries of these quartz c-axis fabrics confirm field observations that define a reversal in shear sense from to
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Kellett, Dawn. "Tectonic Evolution of the South Tibetan Detachment System, Bhutan Himalaya." 2010. http://hdl.handle.net/10222/13153.

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Syn-convergent low-angle normal-sense detachments (LANDs) are found in many orogens around the world. However, those tectonic processes which result in their formation are little known. The South Tibetan detachment system (STDS) is the best-studied example worldwide of a syn-convergent LAND, and formed in the Miocene due to the continental collision of India and Asia. In Bhutan, eastern Himalaya, the STDS is duplicated. Here I investigate the tectonic history of the inner STDS and particularly the outer STDS in Bhutan, to determine whether the duplicated STDS can be explained by or used to con
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Qayyum, Mazhar. "Crustal shortening and tectonic evolution of the Salt Range in Northwest Himalaya, Pakistan /." 1991. http://hdl.handle.net/1957/9504.

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NAGY, CARL. "From cessation of south-directed mid-crust extrusion to onset of orogen-parallel extension, NW Nepal Himalaya." Thesis, 2012. http://hdl.handle.net/1974/7509.

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Field mapping and, structural, microstructural, and chronological analyses confirm the existence of a segment of the Gurla-Mandhata-Humla fault, an orogen-parallel strike-slip dominated shear zone in the upper Karnali valley of northwestern Nepal. This shear zone forms the upper contact of, and cuts obliquely across the Greater Himalayan Sequence (GHS). Data from this study reveal two phases of GHS deformation. Phase 1 is characterized by U-Th-Pb monazite crystallization ages (~26–12 Ma, peak ~18–15 Ma), consistent with typical Neohimalayan metamorphic ages, and the final stages of south-direc
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Lee, Jia-Urnn. "Tectonic episodicity in the greater Himalaya, NW India." Phd thesis, 2013. http://hdl.handle.net/1885/155946.

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The Himalaya is an orogenic welt within the Alpine-Tethyan mountain chain. The extant tectonic model for the Himalayan terrane stack entails continuous post-collisional convergence and persistent heating during burial and subsequent exhumation. An alternative hypothesis to this "continuous evolution" scenario involves episodic tectonic mode switching, a concept that has been documented in other orogens along the Alpine-Tethyan belt. This thesis therefore tests the possibility that there is episodic mode switching in respect to the evolution of the Greater Himalaya in its topographically high c
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Pogue, Kevin R. "Stratigraphic and structural framework of Himalayan foothills, northern Pakistan." Thesis, 1993. http://hdl.handle.net/1957/35578.

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The oldest sedimentary and metasedimentary rocks exposed in the Himalayan foothills of Pakistan record a gradual transition seaward from the evaporites of the Salt Range Formation to pelitic sediments deposited in deeper water to the north. The Upper Proterozoic Tanawal Formation was derived from erosion of a northern highland produced during the early stages of Late Proterozoic to early Ordovician tectonism. Early Paleozoic tectonism is indicated by an angular unconformity at the base of the Paleozoic section, the intrusion of the Mansehra Granite, and the local removal of Cambrian strata. Pa
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Books on the topic "Geology, Structural Kumaun Himalaya"

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Pande, I. C. Tectonic and metamorphic investigations of Kumaon-Garhwal-Himachal Lesser Himalaya. Today & Tomorrow's Printers & Publishers, 1991.

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2

Valdiya, K. S. Geology and natural environment of Nainital Hills, Kumaun Himalaya. Gyānodaya Prakāshan, 1988.

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Dimri, Vijay. Earthquake hazard assessment of Kumaun-Garhwal Himalaya through the application of fractal technique. The Indian Geological Congress, 2003.

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4

India, Geological Survey of, ed. Geology and tectonics of the Himalaya =: Himālaya kā bhūvijñāna evaṃ vivarttanikī. Geological Survey of India, 1989.

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5

Vannay, Jean-Claude. Géologie des chaînes du Haut-Himalaya et du Pir Panjal au Haut-Lahul (NW-Himalaya, Inde): Paléogéographie et tectonique. Impr. Chabloz S.A., 1993.

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Vienna, Austria) Himalaya Karakorum Tibet Workshop (8th 1993. 8th Himalaya Karakorum Tibet Workshop: Vienna, 29.3.--2.4.1993 : abstract volume. Geologische Bundesanstalt, 1993.

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7

Mascle, Georges H. Himalaya-Tibet: La collision continentale Inde-Eurasie. Vuibert, 2010.

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8

Spring, Laurent. Structures gondwaniennes et himalayennes dans la zone tibétaine du Haut Lahul-Zanskar oriental (Himalaya indien). Impr. Chabloz S.A., 1993.

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9

L, Malinconico L., and Lillie R. J, eds. Tectonics of the western Himalayas. edited by Lawrence L. Malinconico and Robert J. Lillie. Geological Association of America, 1990.

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Robyr, Martin. Thrusting, extension and doming in the High Himalaya of Lahul-Zanskar area (NW India): Structural and pressure-temperature constraints. Section des sciences de la terre, Université de Lausanne, 2002.

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Book chapters on the topic "Geology, Structural Kumaun Himalaya"

1

Banerjee, Saikat, Narayan Bose, and Soumyajit Mukherjee. "Field Structural Geological Studies Around Kurseong, Darjeeling-Sikkim Himalaya, India." In Tectonics and Structural Geology: Indian Context. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_16.

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Ali, Asghar, Sajjad Ahmad, Sajjad Ahmad, Mohammad AsifKhan, Muhammad Irfan Khan, and Gohar Rehman. "Tectonic Framework of Northern Pakistan from Himalaya to Karakoram." In Structural Geology and Tectonics Field Guidebook — Volume 1. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60143-0_12.

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Singh, Tejpal, and A. K. Awasthi. "Deformation in the Kangra Reentrant, Himachal Pradesh of NW-Sub Himalaya of India: A Paradox." In Tectonics and Structural Geology: Indian Context. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_13.

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Mahato, Souradeep, Soumyajit Mukherjee, and Narayan Bose. "Documentation of Brittle Structures (Back Shear and Arc-Parallel Shear) from Sategal and Dhanaulti Regions of the Garhwal Lesser Himalaya (Uttarakhand, India)." In Tectonics and Structural Geology: Indian Context. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_15.

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Puniya, Mohit Kumar, and Soumyajit Mukherjee. "Structural Geology Along the Nainital–Pangot Road (Kilbari Section), Nainital Lesser Himalaya (Uttarakhand, India): Focus on Back-Structures." In Structural Geology and Tectonics Field Guidebook — Volume 1. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60143-0_14.

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Ghosh, Rajkumar, and Soumyajit Mukherjee. "Structures of Lesser/Greater Himalaya in and Around an Out-of-Sequence Thrust in the Chaura-Sarahan Area (Himachal Pradesh, India)." In Structural Geology and Tectonics Field Guidebook — Volume 1. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60143-0_13.

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Chauniyal, Devi Datt. "Evidences of Neo-Tectonic Landforms Between Srinagar and Bagwan Area in Lower Alaknanda Valley (Garhwal Himalaya), India." In The Structural Geology Contribution to the Africa-Eurasia Geology: Basement and Reservoir Structure, Ore Mineralisation and Tectonic Modelling. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-01455-1_71.

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