Access the full text.
Sign up today, get DeepDyve free for 14 days.
[Ophiolite and ophiolitic rocks were emplaced along the western, northern and eastern margins of the Indian plate during the northward movement of the Indian plate and the collision of the Indian continental block first with intra-oceanic island arcs within the Neotethys, and then with the Helmand and Kabul continental blocks to the west (Tapponnier et al. 1981), the Asian continental block to the north (Gansser 1964) and the Myanmar continental block to the east (Mitchell 1993)]
Published: Dec 28, 2013
Keywords: Suture Zone; Kink Band; Main Boundary Thrust; Ophiolitic Rock; Undulatory Extinction
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.