geol-amu.org

S. Farooq, Dept of Geology AMU

Economic geology, ore genesis, ore microscopy, mineralogy, plate tectonics, remote sensing and GIS applications, imaging spectroscopy. Since 1980 I have spent much of my research time working in the Himalaya, initially during tenure of a research fellowship of the Wadia. Institute of Himalayan Geology, Dehradun. And subsequently since joining the. Main areas of interest are:. 1 Tectonic Evolution and Metallogeny. In the Himalayan Region. Mineralization in the Askot. 4 Sulfide Mineralization in the Parsoi.

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S. Farooq, Dept of Geology AMU | geol-amu.org Reviews

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Economic geology, ore genesis, ore microscopy, mineralogy, plate tectonics, remote sensing and GIS applications, imaging spectroscopy. Since 1980 I have spent much of my research time working in the Himalaya, initially during tenure of a research fellowship of the Wadia. Institute of Himalayan Geology, Dehradun. And subsequently since joining the. Main areas of interest are:. 1 Tectonic Evolution and Metallogeny. In the Himalayan Region. Mineralization in the Askot. 4 Sulfide Mineralization in the Parsoi.

<META> KEYWORDS

1 s farooq

2 professor

3 department of

4 geology

5 aligarh

6 muslim

7 university

8 india

9 email

10 farooq amu@gmail com

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s farooq,professor,department of,geology,aligarh,muslim,university,india,email,farooq amu@gmail com,teaching areas,research interests,2 petrogenesis,of the askot,crystallines,kumaon,himalaya,3 basemetal,area kumaon,formation of mahakoshal,group,basemetal

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S. Farooq, Dept of Geology AMU | geol-amu.org Reviews

https://geol-amu.org

Economic geology, ore genesis, ore microscopy, mineralogy, plate tectonics, remote sensing and GIS applications, imaging spectroscopy. Since 1980 I have spent much of my research time working in the Himalaya, initially during tenure of a research fellowship of the Wadia. Institute of Himalayan Geology, Dehradun. And subsequently since joining the. Main areas of interest are:. 1 Tectonic Evolution and Metallogeny. In the Himalayan Region. Mineralization in the Askot. 4 Sulfide Mineralization in the Parsoi.

INTERNAL PAGES

geol-amu.org

1

X-eyed stereo view

http://geol-amu.org/exercises/xeyed.htm

Satellite imaging systems that are able to acquire images from at least two different viewing angles can be used for stereomapping. And for generating digital elevation models (DEM). Vast amounts of digital elevation data exist, from large-scale global to smaller scale regional datasets, and many datasets have been merged to improve scale and accuracy. Decisions regarding which data to us for particular. Try to cross-eye view the image below:. To the screen or printed image. Look at the pencil but co...

2

Geology and Structure of the Kumaon Lesser Himalayas

http://geol-amu.org/kumaon/index.htm

We collect, compile and communicate information on the geology and earth resources of Uttarakhand. The Kumaon Himalaya, lying between the Kali River in the east and Sutlej in the west, include a 320 km stretch of mountainous terrain. Much pioneer work was done at the turn of the century followed by more modern investigations between 1930 and 1940. This casts some doubts on certain stratigraphic interpretations. Many workers have postulated existence of the regional inversion of sedimentary pile. Vaikrita...

3

Basemetal Mineralization in Askot, Kumaon Himalaya

http://geol-amu.org/askot/index.htm

Information on the host rocks. Sulfide mineralization occurs in the Precambrian sericite-chlorite schists of pelitic composition at Barigaon near Askot in the Lesser Himalayan region of Kumaon. The schists, forming the lowermost horizon of an inverted sequence of metamorphic rocks, known as the Askot Crystallines, show effects of polymetamorphism - progressive regional type superimposed by dynamic and retrograde type. The thrusting was accompanied by intrusion of dioritic magmas along the thrust plane.

4

X-eyed stereo view

http://geol-amu.org/exercises/anaglyph.htm

Anaglyphs are a class of stereo 3D images created from two photographs taken from two different points (about 2.5 inches apart - the typical distance between human eyes). The. 3D effect is achieved by means of encoding each eye's image using filters of different (usually chromatically opposite) colors, typically. Of the brain fuses this into perception of a three dimensional scene or composition. Anaglyph of Ramgarh Crater. Anaglyph of Lonar Crater. Anaglyph of Vindhyan Rocks of Jhalawar (Rajasthan).

5

S. Farooq, Dept of Geology AMU

http://geol-amu.org/pithoragarh

Basemetal Resource Information System for Pithoragarh District, Kumaon. A Remote Sensing and GIS Approach. Information presented through this website details the findings of a pilot project on the basemetal resources of Pithoragarh district of Uttarakhand, assigned to the author in response to a proposal titled. Basemetal Resource Information System for the Uttaranchal (Kumaon). A Remote Sensing and GIS Approach. Other Resources on the www. To go to the Community Participation Section click here.

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S. Farooq, Dept of Geology AMU

Economic geology, ore genesis, ore microscopy, mineralogy, plate tectonics, remote sensing and GIS applications, imaging spectroscopy. Since 1980 I have spent much of my research time working in the Himalaya, initially during tenure of a research fellowship of the Wadia. Institute of Himalayan Geology, Dehradun. And subsequently since joining the. Main areas of interest are:. 1 Tectonic Evolution and Metallogeny. In the Himalayan Region. Mineralization in the Askot. 4 Sulfide Mineralization in the Parsoi.

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