Petrotectonic significance of the chemistry of chromite in the ultramafic–mafic complexes of Pakistan-Reference-Cited by-同舟云学术

Petrotectonic significance of the chemistry of chromite in the ultramafic–mafic complexes of Pakistan

Published:2006-09 Issue:5 Volume:27 Page:628-646
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Arif Mohammad,Qasim Jan M.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference82 articles.

1. Olistostromal blocks in metamorphosed Saidu mélange, Malakand Agency, North Pakistan;Ahmad,1998

2. Porphyritic, nodular and orbicular chrome ores from Skhakot-Qila complex, Pakistan, and their chemical variations;Ahmed;Mineralogical Magazine,1982

3. Stratigraphic and textural variations in the chromite composition of the ophiolitic Skhakot-Qila complex, Pakistan;Ahmed;Economic Geology,1984

4. Bulk-rock chemistry and petrography of the Skhakot-Qila ophiolite, Pakistan;Ahmed;Acta Mineralogica Pakistanica,1988

5. A supra-subduction zone origin of the Bela ophiolite indicated by the acidic rocks, Khuzdar district, Pakistan;Ahmed;Acta Mineralogica Pakistanica,1991

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