Himalayan tectonics (11 Ergebnisse)

Pamphlet. Zustand: Very Good. Vol 82, pp. 1235-1250, Illus, Extracted from orig vol, thus begins with title page, trimmed & stapled pamphlet, else VG.

Hardcover. Zustand: Very Good. pp.vii, 630 pages, a very good hardback with pictorial laminated boards [0903317923].

11pp, 7 figs, Printed Card Cover, VGC.

28pp, 3 figs, 3 b/w double-page maps, Printed Card Cover, VGC.

Hardcover. Zustand: Very Good-. Light shelf wear to the spine and corners. Two pages have underlining and margin notes in pencil. ; Geological Society Special Publication; 7.25 X 1.25 X 10.25 inches; 630 pages.

8vo, pp. [4], v, [1], 279, [1]; folding charts, tables and maps; cloth-backed boards; hinges cracked, ex-library with spine residue, bookplate, and card pocket, good. A collection of papers presented at the Seminar held on 13-17 September, 1976 in New Delhi. Miscellaneous publication No. 41, part II.…

Taschenbuch. Zustand: Neu. Western Himalayan Foreland Basin, India | Extensional tectonics and climate in pedo-gemorphological and sedimentary evolution of the Western Gangetic Plain, India | Balaji Bhosle (u. a.) | Taschenbuch | 228 S. | Englisch | 2010 | LAP LAMBERT Academic Publishing | EAN 9783838336558 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu.…

1st edition. Geological Society Special Publication No. 74. A very nice copy in tight binding. Used - Very Good. VG hardback in laminated boards (no dust jacket) Used - Very Good. VG hardback in laminated boards (no dust jacket).

Hardcover. Zustand: New. 678 pages. The HimalayaKarakoramTibet mountain belt resulted from Cenozoic collision of India and Asia and is frequently used as the type example of a continental collision orogenic belt. The last quarter of a century has seen the publication of a remarkably detailed dataset relevant to the evolution of this belt. Detailed fieldwork backed up by state-of-the-art structural analysis, geochemistry, mineral chemistry, igneous and metamorphic petrology, isotope chemistry, sedimentology and geophysics produced a wide-ranging archive of data-rich scientific papers. The rationale for this book is to provide a coherent overview of these datasets in addressing the evolution of the mountain ranges we see today. This volume comprises 21 specially invited review papers on the Himalaya, Kohistan arc, Tibet, the Karakoram and Pamir ranges. These papers span the history of Himalayan research, chronology of the collision, stratigraphy, magmatic and metamorphic processes, structural geology and tectonics, seismicity, geophysics, and the evolution of the Indian monsoon. This landmark set of papers should underpin the next 25 years of Himalayan research.…

Zustand: Very Good. Very Good in Very Good dust jacket; Contents are tight and clean; Hard Cover; Oxford & IBH Publishing Co.; 1992; 0.

Taschenbuch. Zustand: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - At ~10ka, all the major rivers in the upper Gangetic plain were incised due to an increase in discharges because of warmer climate, giving rise to large uplands. Compression from SW almost at the same time caused development of curvilinear longitudinal Ganga and Yamuna faults with convexity to the SW, which bounds the study area. Newly developed techniques of remote sensing and GIS are used to identify terminal fans and normal faults in the present flat plains. Ten normal faults nearly normal to the longitudinal faults are identified, indicating their formation related to extensional tectonics. Small streams form terminal fans on the downthrown block of normal faults. GPR studies have provided a facies model for terminal fans. Thus, terminal fans have formed by breaks in slopes caused by faults in contrast to the earlier concept of the loss of discharge by evapo-transpiration. The extensional tectonics playing a major role in shaping the present day landscape in a foreland basin has been brought out convincingly for the first time. Reactivation of the basement features affected surface features in a minor way.…