Himalaya (Geological Aspects). Vol. 2

P. S. Saklani (editor)

Editorial: Satish, 2005
ISBN 10: 8190228986 / ISBN 13: 9788190228985
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660 pp., Hardcover, very good in a very good dust jacket. N° de ref. de la librería

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Título: Himalaya (Geological Aspects). Vol. 2
Editorial: Satish
Año de publicación: 2005
Condición del libro: Very Good

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P S Saklani
ISBN 10: 8190228986 ISBN 13: 9788190228985
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Descripción Hardcover. Estado de conservación: Like New. Unread, very minor shelf wear. Nº de ref. de la librería HBS-00240719-B

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P.S. Saklani
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Descripción Satish Serial Publishing House, 2005. Hardcover. Estado de conservación: New. book. Nº de ref. de la librería M8190228986

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P S Saklani
Editorial: Satish Serial Publishing House, Delhi
ISBN 10: 8190228986 ISBN 13: 9788190228985
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Descripción Satish Serial Publishing House, Delhi. Hardcover. Estado de conservación: NEW. Very light use, very minor shelf wear. Nº de ref. de la librería HBS-00027394-B

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P.S. Saklani (Ed.)
Editorial: Satish Serial Publishing House (2005)
ISBN 10: 8190228986 ISBN 13: 9788190228985
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Descripción Satish Serial Publishing House, 2005. Hardcover. Estado de conservación: New. The volume is mainly focussed on structural and metamorphic characteristics of the Himalayan rocks exposed in various sectors of the Himalaya. The peridotites in the Spongtang nappe of Ladakh are mylonitised and occur in superposed imbrications. The regionally metamorphosed pelitic rocks of a part of Kashmir show low pressure, intermediate and medium pressure of metamorphism. The Buniyar granite is an intrusive plunton in the Dogra Slates (Precambrian) in the western part of Kashmir. The NE-SW compressional stress was responsible for development of multiple folds in metamorphics of Chamba area. The radiometric date of granites in Chor mountain is Pre-tertiary (1000 m.y and 525 m.y.). The metamorphic and folding processes of the Chor pelites were terminated by the Jutogh thrusting phenomena. The crystallines of Palampur (Himachal) are characterised by the Chail thrust and contain about 12 types of garnet texturally. The Manali-Rohtang Pass area forms a part of an overturned limb of the crystalline nappe. The thrusts in the Kumaun region developed from the hinterland to foreland. The total displacement of the Munsiari, Krol and Berinag sheets was about 330 km. The Purola area in Garhwal is located between the Main Central Thrust and Tons Thrust. Metamorphics in the Bhagirathi valley were formed at the temperatures ranging from 479 to 666 c. The uranium mineralisation in the granite-gneisses and the footwall quartzite took place after the formation of the Main Central Thrust III in Tehri Garhwal. The rock-fabric (b-c girdles of quartz) in rocks of Lansdowne crystalline nappe developed along the thrust-transport direction with rotation which is exhibited by triclinic symmetry. The fracture and lineament patterns were formed in the frontal parts of the Himalaya. The Lesser Himalaya region in Himachal Pradesh has overlapping crystalline thrust. The chail nappes are traceable throughout the length of the Lesser Himalaya. The nappe thrusting in two phases occurred in Eastern Nepal during middle tertiary and quaternary times. Simple shear type of deformation affected the rocks in Eastern Nepal. The high heat flow in rocks of Darjiling region was responsible for the first phase of metamorphism which was followed by overturning and thrusting during the second phase of deformation. The metapelites in Eastern Sikkim are characterised by Kyanite-sillimanite isograd with associated quartzofeldspathic melt during pre-and syn-kinematic deformation. The reflected Aravalli trends and present in Arun transanticline and Tista Dome in Bhutan. The Central Tibetan region was possibly the homeland for the nappes in the Eastern Himalaya. This book would be useful to earth scientists, academicians and research scholars. Printed Pages: 660. Nº de ref. de la librería 64432

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P.S. Saklani (Ed.)
Editorial: Satish Serial Publishing House (2005)
ISBN 10: 8190228986 ISBN 13: 9788190228985
Nuevos Tapa dura Cantidad: > 20
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A - Z Books
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Descripción Satish Serial Publishing House, 2005. Hardcover. Estado de conservación: New. The volume is mainly focussed on structural and metamorphic characteristics of the Himalayan rocks exposed in various sectors of the Himalaya. The peridotites in the Spongtang nappe of Ladakh are mylonitised and occur in superposed imbrications. The regionally metamorphosed pelitic rocks of a part of Kashmir show low pressure, intermediate and medium pressure of metamorphism. The Buniyar granite is an intrusive plunton in the Dogra Slates (Precambrian) in the western part of Kashmir. The NE-SW compressional stress was responsible for development of multiple folds in metamorphics of Chamba area. The radiometric date of granites in Chor mountain is Pre-tertiary (1000 m.y and 525 m.y.). The metamorphic and folding processes of the Chor pelites were terminated by the Jutogh thrusting phenomena. The crystallines of Palampur (Himachal) are characterised by the Chail thrust and contain about 12 types of garnet texturally. The Manali-Rohtang Pass area forms a part of an overturned limb of the crystalline nappe. The thrusts in the Kumaun region developed from the hinterland to foreland. The total displacement of the Munsiari, Krol and Berinag sheets was about 330 km. The Purola area in Garhwal is located between the Main Central Thrust and Tons Thrust. Metamorphics in the Bhagirathi valley were formed at the temperatures ranging from 479 to 666 c. The uranium mineralisation in the granite-gneisses and the footwall quartzite took place after the formation of the Main Central Thrust III in Tehri Garhwal. The rock-fabric (b-c girdles of quartz) in rocks of Lansdowne crystalline nappe developed along the thrust-transport direction with rotation which is exhibited by triclinic symmetry. The fracture and lineament patterns were formed in the frontal parts of the Himalaya. The Lesser Himalaya region in Himachal Pradesh has overlapping crystalline thrust. The chail nappes are traceable throughout the length of the Lesser Himalaya. The nappe thrusting in two phases occurred in Eastern Nepal during middle tertiary and quaternary times. Simple shear type of deformation affected the rocks in Eastern Nepal. The high heat flow in rocks of Darjiling region was responsible for the first phase of metamorphism which was followed by overturning and thrusting during the second phase of deformation. The metapelites in Eastern Sikkim are characterised by Kyanite-sillimanite isograd with associated quartzofeldspathic melt during pre-and syn-kinematic deformation. The reflected Aravalli trends and present in Arun transanticline and Tista Dome in Bhutan. The Central Tibetan region was possibly the homeland for the nappes in the Eastern Himalaya. This book would be useful to earth scientists, academicians and research scholars. Printed Pages: 660. Nº de ref. de la librería 64432

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Editorial: Satish Serial Publishing House
ISBN 10: 8190228986 ISBN 13: 9788190228985
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Descripción Satish Serial Publishing House. Estado de conservación: New. pp. 660 , , , Nº de ref. de la librería 7720547

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P.S. Saklani
Editorial: Satish Serial Publishing House, Delhi (2005)
ISBN 10: 8190228986 ISBN 13: 9788190228985
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Descripción Satish Serial Publishing House, Delhi, 2005. Hardcover. Estado de conservación: New. Nº de ref. de la librería 359835

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P S Saklani
Editorial: Satish Serial Pub (2005)
ISBN 10: 8190228986 ISBN 13: 9788190228985
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Descripción Satish Serial Pub, 2005. Hardcover. Estado de conservación: As New. Dust Jacket Included. Contents 1. The Central Himalayan gneisses in Northern Pakistan/R.D. Broughton and B.F. Windley. 2. Ductile shearing in peridotites of spongtang Nappe Ladakh/I. Reuber P. Nehlig and G. Reibel. 3. Low pressure metamorphism in a regionally metamorphic terrain of Doda Kashmir Himalaya/B.K. Das. 4. The Buniyar Granite of the Kashmir Himalaya/T.R. Sharma and K.R. Sharma. 5. The aureole zone and metasediments of Dhauladhar Chaori Khas (H.P.)/R.S. Bedi and A.K. Prasad. 6. Geochronology of Bandal Granitoids Kulu Himachal Pradesh/N. Kishore V.P. Singh A.K. Kansal A. Kumar N.K. Sharma and Bimal Rai. 7. The Jutoghs and their structural history Chur Area/R.C. Kanwar and I. Singh. 8. Garnets and metapelites of the Palampur Area (H.P.)/N. Chaudhri and L.N. Gupta. 9. Metamorphics of Manali Rohtang area NW Himalaya/S. Kumar. 10. Structural analysis of Chamba region Himachal Pradesh/B.K. Sharma and A.M. Bhola 11. Structures of Purola area Garhwal Himalaya/A.K. Pachauri. 12. Mylonites of Dunda area Uttarakashi Uttaranchal/R.K. Prasad. 13. Metamorphics of the Bhagirathi valley Garhwal Himalaya/P.S. Saklani and V.K. Bahuguna. 14. Uranium mineralisation around Raunsal Uttaranchal/G.R. Narayan Das G.S. Bhatnagar A.K. Bhattacharya and Y.C. Sharma. 15. Naini group/Nappe Rudraprayag (Garhwal Himalaya)/S. Varadarajan and R.S. Rawat. 16. Fabric of the Amri tectonites Lansdowne area Uttaranchal/S.N. Sarkar and S.M. Dutta. 17. Tectonics of Central crystallines Nappes Garhwal Himalaya/P.S. Saklani. 18. Reinterpretation of the tectonics of the Central and Southern Lesser Himalaya Uttaranchal/V.K. Gairola. 19. Structural evolution of the Kumaun Lesser Himalaya/M.R.W. Johnson. 20. Structure of the Kumaun Lesser Himalaya/K.S. Valdiya. 21. Central crystallines and main central thrust Eastern Kumaun Himalaya/V.C. Thakur and B.K. Choudhury. 22. The North Almora Thrust zone Kumaun Himalaya/D.B. Yedekar and K.B. Powar. 23. Fractures and lineaments in the Lesser Himalaya of Kumaun/R.N. Pande G. Dikshit and D.N. Kanungo. 24. The Chail Nappes in the Himalaya/G. Fuchs. 25. Chail metamorphics of the Himachal Pradesh/N.S. Virdi. 26. Relief thrusts in the Eastern Nepal Himalaya/J. Jaros and J. Kalvoda. 27. Structure and metamorphism in Eastern Nepal/Y. Maruo and K. Kizaki. 28. Mesoscopic structures and tectonics of the Central Nepal Himalaya/W. Bogacz and J. Krokowski. 29. Barrovian metamorphism of Takdah Darjeeling (Eastern Himalaya)/R.K. Lal S. Mukerji and D. Ackermand. 30. Deformation and strain of the Himalayan Nappes Sikkim Eastern Himalaya/S. Sinha Roy. 31. The Bhutan Himalaya stratigraphy and structure/B.S. Jangpangi. 32. Eastern Himalayan stratigraphy and tectonics/S.K. Acharyya. 33. Structural geology of the Siyom Valley Arunachal Pradesh/Surendra Singh and A.K. De. The volume is mainly focussed on structural and metamorphic characteristics of the Himalayan rocks exposed in various sectors of the Himalaya. The peridotites in the Spongtang nappe of Ladakh are mylonitised and occur in superposed imbrications. The regionally metamorphosed pelitic rocks of a part of Kashmir show low pressure intermediate and medium pressure of metamorphism. The Buniyar granite is an intrusive plunton in the Dogra Slates (Precambrian) in the western part of Kashmir. The NE SW compressional stress was responsible for development of multiple folds in metamorphics of Chamba area. The radiometric date of granites in Chor mountain is Pre tertiary (1000 m.y and 525 m.y.). The metamorphic and folding processes of the Chor pelites were terminated by the Jutogh thrusting phenomena. The crystallines of Palampur (Himachal) are characterised by the Chail thrust and contain about 12 types of garnet texturally. The Manali Rohtang Pass area forms a part of an overturned limb of the crystalline nappe. The thrusts in the Kumaun region developed from the hinterland to foreland. The total displacement of the Munsiari Krol and Berinag sheets was about 330 km. The Purola area in Garhwal is located between. Nº de ref. de la librería 54626

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