TY - JOUR
T1 - Water-rock interaction in Krafla and Reykjanes geothermal systems, Iceland.
AU - Sveinbjörnsdóttir, Árný Erla
N1 - © Copyright 2018 Elsevier B.V., All rights reserved.
PY - 1983/8
Y1 - 1983/8
N2 - The Reykjanes hydrothermal system contains a highly saline (Cl 19 260 ppm) circulating fluid at depth, due to influx of sea-water, whereas at Krafla the fluid is non-saline meteoric water. Extensive oxygen isotope exchange has occurred between the hydrothermal altered rock and the circulating fluid in the Krafla geothermal field. The Krafla hydrothermal fluid has delta 18O = - 11.9per mille and delta D = -86.8per mille. -R.A.H.
AB - The Reykjanes hydrothermal system contains a highly saline (Cl 19 260 ppm) circulating fluid at depth, due to influx of sea-water, whereas at Krafla the fluid is non-saline meteoric water. Extensive oxygen isotope exchange has occurred between the hydrothermal altered rock and the circulating fluid in the Krafla geothermal field. The Krafla hydrothermal fluid has delta 18O = - 11.9per mille and delta D = -86.8per mille. -R.A.H.
UR - http://www.scopus.com/inward/record.url?scp=0021083951&partnerID=8YFLogxK
U2 - 10.1144/gsjgs.140.4.0549
DO - 10.1144/gsjgs.140.4.0549
M3 - Article
AN - SCOPUS:0021083951
SN - 0016-7649
VL - 140
SP - 549
EP - 550
JO - Journal of the Geological Society
JF - Journal of the Geological Society
IS - 4
ER -