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The document summarizes a study of the Waziristan ophiolite complex in Pakistan. It describes the general geology, including that the ophiolite was tectonically emplaced in the Paleocene to early Eocene era. It consists of typical ophiolite rocks like ultramafic rocks, gabbros, sheeted dikes, pillow lavas, and pelagic sediments, though the sequence is not complete in any single locality due to tectonic dismemberment. The study also analyzes the mineral chemistry of chromitites found within the complex.

Author

noor abdullah

Language

EN