Seafloor hydrothermal systems driven by the serpentinization of peridotite
نویسندگان
چکیده
منابع مشابه
30,000 years of hydrothermal activity at the lost city vent field.
Strontium, carbon, and oxygen isotope data and radiocarbon ages document at least 30,000 years of hydrothermal activity driven by serpentinization reactions at Lost City. Serpentinization beneath this off-axis field is estimated to occur at a minimum rate of 1.2 x 10(-4) cubic kilometers per year. The access of seawater to relatively cool, fresh peridotite, coupled with faulting, volumetric exp...
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A simple model of reaction-induced cracking applied to serpentinization and carbonation of peridotite
Article history: Received 8 July 2009 Received in revised form 6 November 2009 Accepted 8 January 2010 Available online 2 February 2010
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ژورنال
عنوان ژورنال: Geophysical Research Letters
سال: 2002
ISSN: 0094-8276
DOI: 10.1029/2001gl014411