A continental forearc serpentinite diapir with deep origins: Elemental signatures of a mantle wedge protolith and slab-derived fluids at New Idria, California
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چکیده
منابع مشابه
Troodos: A Giant Serpentinite Diapir
Troodos is a classical ophiolite complex. It is proposed that the serpentinized harzburgites that now form the top of the mountain and represent the originally lowest part of the ophiolite sequence rose as a diapir. This diapiric rise is caused by the pervasive serpentinization of a suboceanic harzburgite, due to rock-sea water interaction. The serpentinization caused a 44% expansion of the roc...
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ژورنال
عنوان ژورنال: Lithos
سال: 2021
ISSN: 0024-4937
DOI: 10.1016/j.lithos.2021.106252