Infra‐arc mantle–crust transition and intra‐arc mantle diapirs in the Kohistan Complex (Pakistani Himalaya): petro‐structural evidence-Reference-Cited by-同舟云学术

Infra‐arc mantle–crust transition and intra‐arc mantle diapirs in the Kohistan Complex (Pakistani Himalaya): petro‐structural evidence

Author:

Burg ¹,Bodinier ²,Chaudhry ³,Hussain ⁴,Dawood ⁴

Affiliation:

1. Geologisches Institut, ETH‐Zentrum, Sonneggstrasse 5, CH‐8092 Zürich, Switzerland.

2. UMR C5569, ISTEEM, Université Montpellier 2, Place E. Bataillon, Cc 57, 34095 Montpellier Cédex 05, France.

3. Institute of Geology, Punjab University, Quaid‐e‐Azam Campus, 54590 Lahore, Pakistan.

4. Pakistan Museum of Natural History, Garden Avenue, Shakarparian, Islamabad 44000, Pakistan.

Publisher

Wiley

Subject

Geology

Link

Reference33 articles.

1. Chronology of subduction, collision and regional metamorphism in Kohistan, NW Himalaya, Pakistan.;Anczkiewicz R.;Terra Abstracts,1997

3. The Kohistan sequence: crust and mantle of an obducted island arc.;Bard J.‐P.;Geol. Bull. Univ. Peshawar,1980

5. Bender F.K.&Raza H.A. 1995.Geology of Pakistan. Betreige zur regionalen Geologie der Erde 25. Gebrüder Borntraeger Berlin 414pp.

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