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Evolution of fluid–rock interaction in the Reykjanes geothermal system, Iceland: Evidence from Iceland Deep Drilling Project core RN-17B

Journal Article · · Journal of Volcanology and Geothermal Research
 [1];  [1];  [1];  [2];  [3]
  1. Univ. of California, Davis, CA (United States)
  2. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
  3. HS Orka, Reykjanesbaer (Iceland)
We describe the lithology and present spatially resolved geochemical analyses of samples from the hydrothermally altered Iceland Deep Drilling Project (IDDP) drill core RN-17B. The 9.3 m long RN-17B core was collected from the seawater-dominated Reykjanes geothermal system, located on the Reykjanes Peninsula, Iceland. The nature of fluids and the location of the Reykjanes geothermal system make it a useful analog for seafloor hydrothermal processes, although there are important differences. Here, the recovery of drill core from the Reykjanes geothermal system, as opposed to drill cuttings, has provided the opportunity to investigate evolving geothermal conditions by utilizing in-situ geochemical techniques in the context of observed paragenetic and spatial relationships of alteration minerals.
Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
National Science Foundation (NSF); USDOE National Nuclear Security Administration (NNSA)
Grant/Contract Number:
AC52-07NA27344
OSTI ID:
1840846
Alternate ID(s):
OSTI ID: 1879269
Report Number(s):
LLNL-JRNL--818931; LLNL-JRNL-693298; 1029798
Journal Information:
Journal of Volcanology and Geothermal Research, Journal Name: Journal of Volcanology and Geothermal Research Vol. 302; ISSN 0377-0273
Publisher:
ElsevierCopyright Statement
Country of Publication:
United States
Language:
English

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