Petrology and geochemistry of mantle peridotites from the Kalaymyo and Myitkyina ophiolites (Myanmar): Implications for tectonic settings
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文摘

Mantle peridotites from the Kalaymyo and Myitkyina ophiolites in Myanmar have been studied.

The Kalaymyo spinel lherzolites have been subjected to 3–15% degrees of fractional melting.

Spinel harzburgites from both ophiolites have experienced 11–21% degrees of fractional melting.

Refractory harzburgites from both ophiolites have experienced hydrous melting.

Both MOR- and SSZ-type peridotites crop out in the Kalaymyo and Myitkyina ophiolites.

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