Is the Troodos ophiolite (Cyprus) a complete, transform fault–bounded Neotethyan ridge segment?-Reference-Cited by-同舟云学术

Is the Troodos ophiolite (Cyprus) a complete, transform fault–bounded Neotethyan ridge segment?

Published:2016-02-05 Issue:3 Volume:44 Page:199-202
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:Geology

Author:

Morris Antony,Maffione Marco

Publisher

Geological Society of America

Subject

Geology

Reference37 articles.

1. Evidence from gabbro of the Troodos ophiolite for lateral magma transport along a slow-spreading mid-ocean ridge

2. Fault block rotations in ophiolites: Results of palaeomagnetic studies in the Troodos Complex, Cyprus;Allerton;Paleomagnetic Rotations and Continental Deformation: NATO Advanced Science Institutes Series C,1989

3. Distortions, rotations and crustal thinning at ridge–transform intersections

4. Spreading structure of the Troodos ophiolite, Cyprus: Some paleomagnetic constraints

5. Allerton, S. , Vine, F.J. , 1990, Palaeomagnetic and structural studies of the southeastern part of the Troodos complex, in Malpas, J. ., eds., Ophiolites: Oceanic Crustal Analogues: Nicosia, Cyprus Geological Survey Department, p. 99–111.

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