Petromagnetic Characteristics of Serpentinization and Magnetite Formation at the Zedang Ophiolite in Southern Tibet

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2020.

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Abstract:

Variably serpentinized peridotites from the Zedang ophiolite in southern Tibet were magnetically and petrologically examined to understand the serpentinization process and evaluate the origin of magnetic anomalies in ultramafic-hosted tectonic settings. Magnetite occurs in the serpentine and brucite veins and is identified as the dominant...More

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