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Tuesday, May 12, 2020 | History

2 edition of Geologic and Tectonic Maps of the Himalayan Region found in the catalog.

Geologic and Tectonic Maps of the Himalayan Region

A. Gansser

Geologic and Tectonic Maps of the Himalayan Region

by A. Gansser

  • 362 Want to read
  • 10 Currently reading

Published by John Wiley and Sons Ltd .
Written in English


The Physical Object
FormatHardcover
ID Numbers
Open LibraryOL10295707M
ISBN 100470290579
ISBN 109780470290576

Download file to see previous pages The Himalayas are mountain range in asia separating the indian sub continent and tibetan plateau. The meaning of the word Himalaya in sanskrit is "abode of the snow." The geology of the Himalayan mountain is the most dramatic and . Geology of the Himalayan Belt: Deformation, Metamorphism, Stratigraphy. presents sophisticated metamorphic and igneous rock data across various Himalayan geographic sectors, capturing their petrography, metamorphism, structure, mineralization, and regional tectonic research.. With an east-west extension of about kilometers and numerous meter peaks, the Himalayas are the most.

Geoscientists directly or indirectly associated with the Wadia Institute of Himalayan geology have worked between the extreme NW end of the Himalaya in Ladakh and the eastern extremity in Arunachal Pradesh (Fig. 1); this paper summarizes their by: 6. The ihsan Ketin NATO Advanced Study Institute on the Tectonic Evolution of the Tethyan Region was conceived in in Veszprem, Hungary, when three of the organizers (B. C. B., L. H. R. and A. M. C. 9.) had come together for a meeting on the tectonics of the Pannonian basin.

The geology of Nepal is dominated by the Himalaya, the highest, youngest and a very highly active mountain range (Upreti , p. 1).Himalaya is a type locality for the study of on-going continent-continent collision tectonics (Upreti , p. 1).The Himalayan arc extends about 2, km (1, mi) from Nanga Parbat (8, m (26, ft)) by the Indus River in northern Pakistan eastward to. geology of nepal himalaya The Himalaya range is about km. long and extends from Indus rive of Pakistan in the west to Assam in east. The Himalaya belt is the results of collision of two tectonic plates, Indian plate and Tibetan plate on the north.


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Geologic and Tectonic Maps of the Himalayan Region by A. Gansser Download PDF EPUB FB2

In the last 15 years there has been an explosion of data and theories from both geological and geophysical perspectives. This book presents the results of integrated multidisciplinary studies, including geology, petrology, magmatism, geochemistry, geochronology and geophysics, of the structures and processes affecting the continental lithosphere.

Geologic and tectonic maps of the Himalayan region / prepared by A. Gansser | National Library of Australia Due to the need to contain the spread of coronavirus (COVID) the Library building and reading rooms are closed to visitors until further notice.

This book addresses the geology of the entire Himalayan range in Nepal, i.e., from the Gangetic plain in the south to the Tethyan zone in the north. Without a comprehensive look at the various Himalayan zones, it is practically impossible to fully grasp the processes at work behind the formation and development of the spectacular : Springer International Publishing.

Accompanied by booklet 'Explanations of the geologic-tectonic map of the Himalaya by Gerald Fuchs with 13 figures and 1 plate'.

Vienna: Geological survey of Austria, 50p cm. ISBN ; and loose Plate 1: The evolution of Zanskar and the Indus Zone, coloured cross-sections, 29cm x 22 cm, folded to 15cm x 22 cm. Abstract. The geology and tectonics of the Himalaya has been reviewed in the light of new data and recent studies by the author.

The data suggest that the Lesser Himalayan Gneissic Basement (LHGB) represents the northern extension of the Bundelkhand craton, Northern Indian shield and the large scale granite magmatism in the LHGB towards the end of the Palæoproterozoic Wangtu Orogeny Cited by: understanding of the geology of the Himalayan mountain and a better constrained model of its geodynamic evolution.

Despite the fact that many gaps in the under- standing of the Himalayan geology and its tectonic evolution, have been filled, there are still many grey areas in. Map of northern Pakistan showing the location of the mapped area and the structural trend lines of the region.

Geologic map of the southern Himalaya in Hazara, Pakistan, and adjacent areas. Reconnaissance geologic map and sections of the Tarbela area, Pakistan. Geologic map and sections of the Garhi Habibullah area, Hazara district, by:   To address this issue, we conducted detailed field mapping, U-Pb zircon age dating, and 40Ar/39Ar thermo chronology along two geologic traverses at longitudes of 92°E and 94°E across the eastern Himalaya.

Our dating indicates the region experienced magmatic events at Ma, Ma, Ma, and by: This report on Himalayan Geology covers its mode of formation, glaciation and quaternary geology, current tectonics and resources.

It will also outline aspects specific to Ladakh as this report was commissioned by Geology for Global Development as part of a geo-hazards education project in the Ladakh region. The Himalayas formed in two stages.

The Himalayas are a prime example of how tectonic plate motion can manipulate the earth in extraordinary ways. These colliding plates resulted in the formation of the highest mountain range on the. "These maps have been reprinted from Geology of the Himalayas, by Professor A.

Gansser, University of Zurich, Switzerland."--Accompanying text. Plate 1 includes ancillary map: Tectonic map of the Himalayas and surrounding areas. The Buxa Group is exposed all along the lower hills of Bhutan Himalaya. The Shumar–Daling Group of rocks overlies the Buxa sequence and occurs all along the upper tectonic levels of the Lesser Himalayan belt of Bhutan.

The higher grade Thimphu Group overlies. Title: Geology and geodynamic evolution of the Himalayan collision zone, Vol Parts Physics and chemistry of the earth Geology and Geodynamic Evolution of the Himalayan Collision Zone, Kewal K.

Sharma: Editor. Metamorphic, magmatic, and tectonic evolution of the central Karakoram in the Biafo-Baltoro-Hushe regions of northern Pakistan Author(s) M. Searle. Buy Tectonics of the Himalaya (): NHBS - Soumyajit Mukherjee, Rodolfo Carosi, Peter A van der Beek, Barun Kumar Mukherjee, Delores M Robinson, Geological Society.

This book compiles and synthesizes the post data of the Western Himalaya. The geology of Western Himalaya is described under a tectonic zone framework, and wherever necessary, different. This book addresses the geology of the entire Himalayan range in Nepal, i.e., from the Gangetic plain in the south to the Tethyan zone in the north.

Without a comprehensive look at the various Himalayan zones, it is practically impossible to fully grasp the processes at work behind the formation and development of the spectacular by:   A detailed Map explaining the Plate Tectonics and the Geology of the Himalayas and their formation.

Helps us understand the basic fault lines between the Indian and the Eurasian Plate. Many other smaller details make it a good guide to understanding the formation and the evolution of the Himalayas. Here, ascale geological map of the central Himalaya of Western Region, Nepal is presented.

This map represents a compilation of previously published maps, integrated with new geological. This book compiles and synthesizes the post data of the Western Himalaya.

The geology of Western Himalaya is described under a tectonic zone framework, and wherever necessary, different regions are discussed separately under each tectonic zone.

A geological map of the Western Himalaya has been compiled onscale. Following field mapping of the metamorphic sequences in central Himalayas (e.g. Nepal, Sikkim and Bhutan) in the last 20 years we can observe a clear evolution from the classical geological maps, mainly based on field work, towards a new generation of geological maps based on integrated field work, remote sensing, meso- and micro-structural analysis, petrology and in situ by: The Himalaya, located on the southern fringe of the Tibetan Plateau, form a mountain arc (convex toward the south) about km long and km wide; they are bounded by two structural bends on the northwest (Nanga Parbat, the Indus gorge) and northeast (Namcha Barwa, the Tsangpo gorge).

The Himalaya are the loftiest and still rising mountains in the world.The Himalayan tectonic system consists of features produced by the Cenozoic Indo-Asian collision, the Himalayan orogen, the active Himalayan foreland basin and the Indus and Bengal fans.

The Himalayan Foreland basin is a broad, “up-side down U-shaped” basin in map .