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

Andrew P.G. Fowler; Robert A. Zierenberg; Peter Schiffman; Naomi Marks; Gumundur Ómar Frileifsson

doi:10.1016/j.jvolgeores.2015.06.009

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

Andrew P.G. Fowler, Robert A. Zierenberg, Peter Schiffman, Naomi Marks, Gumundur Ómar Frileifsson

Research output: Contribution to journal › Article › peer-review

12 Scopus citations

Abstract

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 9.3m 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. 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. The RN-17B core was returned from a vertical depth of ~2560m and an in-situ temperature of ~345°C. The primary lithologies are basaltic in composition and include hyaloclastite breccia, fine-grained volcanic sandstone, lithic breccia, and crystalline basalt. Primary igneous phases have been entirely pseudomorphed by calcic plagioclase+magnesium hornblende+chlorite+titanite+albitized plagioclase+vein epidote and sulfides. Despite the extensive hydrothermal metasomatism, original textures including hyaloclastite glass shards, lithic clasts, chilled margins, and shell-fragment molds are superbly preserved. Multi-collector LA-ICP-MS strontium isotope ratio (⁸⁷Sr/⁸⁶Sr) measurements of vein epidote from the core are consistent with seawater as the dominant recharge fluid. Epidote-hosted fluid inclusion homogenization temperature and freezing point depression measurements suggest that the RN-17B core records cooling through the two-phase boundary for seawater over time to current in-situ measured temperatures. Electron microprobe analyses of hydrothermal hornblende and hydrothermal plagioclase confirm that while alteration is of amphibolite-grade, it is in disequilibrium and the extent of alteration is dependent upon protolith type and water/rock ratio. Alteration in the RN-17B core bares many similarities to that of Type II basalts observed in Mid-Atlantic Ridge samples.

Original language	English (US)
Pages (from-to)	47-63
Number of pages	17
Journal	Journal of Volcanology and Geothermal Research
Volume	302
DOIs	https://doi.org/10.1016/j.jvolgeores.2015.06.009
State	Published - Sep 1 2015
Externally published	Yes

Bibliographical note

Funding Information:
RN-17B was recovered at considerable expense, thanks in large part to funding from NSF's Continental Dynamics Program. The research described herein was supported by the National Science Foundation grant EAR 0507518 . Samples for this study were provided by IDDP. I would like to thank Qin-Zhu Yin and Josh Wimpeny for coordinating access to the LA-MC-ICP-MS facility at UC Davis. I would also like to thank HS Orka for their hospitality and for providing access to drill core samples at the Reykjanes geothermal field.

Publisher Copyright:
© 2015 Elsevier B.V.

Keywords

Epidote
Geothermal
Hydrothermal alteration
Iceland
RN-17B Drill Core
Reykjanes

Access

10.1016/j.jvolgeores.2015.06.009

Cite this

Evolution of fluid-rock interaction in the Reykjanes geothermal system, Iceland : Evidence from Iceland Deep Drilling Project core RN-17B. / Fowler, Andrew P.G.; Zierenberg, Robert A.; Schiffman, Peter; Marks, Naomi; Frileifsson, Gumundur Ómar.

In: Journal of Volcanology and Geothermal Research, Vol. 302, 01.09.2015, p. 47-63.

Research output: Contribution to journal › Article › peer-review

@article{a7122e73090045fe90c9d762e52a8560,

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

abstract = "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 9.3m 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. 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. The RN-17B core was returned from a vertical depth of ~2560m and an in-situ temperature of ~345°C. The primary lithologies are basaltic in composition and include hyaloclastite breccia, fine-grained volcanic sandstone, lithic breccia, and crystalline basalt. Primary igneous phases have been entirely pseudomorphed by calcic plagioclase+magnesium hornblende+chlorite+titanite+albitized plagioclase+vein epidote and sulfides. Despite the extensive hydrothermal metasomatism, original textures including hyaloclastite glass shards, lithic clasts, chilled margins, and shell-fragment molds are superbly preserved. Multi-collector LA-ICP-MS strontium isotope ratio (87Sr/86Sr) measurements of vein epidote from the core are consistent with seawater as the dominant recharge fluid. Epidote-hosted fluid inclusion homogenization temperature and freezing point depression measurements suggest that the RN-17B core records cooling through the two-phase boundary for seawater over time to current in-situ measured temperatures. Electron microprobe analyses of hydrothermal hornblende and hydrothermal plagioclase confirm that while alteration is of amphibolite-grade, it is in disequilibrium and the extent of alteration is dependent upon protolith type and water/rock ratio. Alteration in the RN-17B core bares many similarities to that of Type II basalts observed in Mid-Atlantic Ridge samples.",

keywords = "Epidote, Geothermal, Hydrothermal alteration, Iceland, RN-17B Drill Core, Reykjanes",

author = "Fowler, {Andrew P.G.} and Zierenberg, {Robert A.} and Peter Schiffman and Naomi Marks and Frileifsson, {Gumundur {\'O}mar}",

note = "Funding Information: RN-17B was recovered at considerable expense, thanks in large part to funding from NSF's Continental Dynamics Program. The research described herein was supported by the National Science Foundation grant EAR 0507518 . Samples for this study were provided by IDDP. I would like to thank Qin-Zhu Yin and Josh Wimpeny for coordinating access to the LA-MC-ICP-MS facility at UC Davis. I would also like to thank HS Orka for their hospitality and for providing access to drill core samples at the Reykjanes geothermal field. Publisher Copyright: {\textcopyright} 2015 Elsevier B.V.",

year = "2015",

month = sep,

day = "1",

doi = "10.1016/j.jvolgeores.2015.06.009",

language = "English (US)",

volume = "302",

pages = "47--63",

journal = "Journal of Volcanology and Geothermal Research",

issn = "0377-0273",

publisher = "Elsevier",

}

TY - JOUR

T1 - Evolution of fluid-rock interaction in the Reykjanes geothermal system, Iceland

T2 - Evidence from Iceland Deep Drilling Project core RN-17B

AU - Fowler, Andrew P.G.

AU - Zierenberg, Robert A.

AU - Schiffman, Peter

AU - Marks, Naomi

AU - Frileifsson, Gumundur Ómar

N1 - Funding Information: RN-17B was recovered at considerable expense, thanks in large part to funding from NSF's Continental Dynamics Program. The research described herein was supported by the National Science Foundation grant EAR 0507518 . Samples for this study were provided by IDDP. I would like to thank Qin-Zhu Yin and Josh Wimpeny for coordinating access to the LA-MC-ICP-MS facility at UC Davis. I would also like to thank HS Orka for their hospitality and for providing access to drill core samples at the Reykjanes geothermal field. Publisher Copyright: © 2015 Elsevier B.V.

PY - 2015/9/1

Y1 - 2015/9/1

N2 - 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 9.3m 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. 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. The RN-17B core was returned from a vertical depth of ~2560m and an in-situ temperature of ~345°C. The primary lithologies are basaltic in composition and include hyaloclastite breccia, fine-grained volcanic sandstone, lithic breccia, and crystalline basalt. Primary igneous phases have been entirely pseudomorphed by calcic plagioclase+magnesium hornblende+chlorite+titanite+albitized plagioclase+vein epidote and sulfides. Despite the extensive hydrothermal metasomatism, original textures including hyaloclastite glass shards, lithic clasts, chilled margins, and shell-fragment molds are superbly preserved. Multi-collector LA-ICP-MS strontium isotope ratio (87Sr/86Sr) measurements of vein epidote from the core are consistent with seawater as the dominant recharge fluid. Epidote-hosted fluid inclusion homogenization temperature and freezing point depression measurements suggest that the RN-17B core records cooling through the two-phase boundary for seawater over time to current in-situ measured temperatures. Electron microprobe analyses of hydrothermal hornblende and hydrothermal plagioclase confirm that while alteration is of amphibolite-grade, it is in disequilibrium and the extent of alteration is dependent upon protolith type and water/rock ratio. Alteration in the RN-17B core bares many similarities to that of Type II basalts observed in Mid-Atlantic Ridge samples.

AB - 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 9.3m 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. 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. The RN-17B core was returned from a vertical depth of ~2560m and an in-situ temperature of ~345°C. The primary lithologies are basaltic in composition and include hyaloclastite breccia, fine-grained volcanic sandstone, lithic breccia, and crystalline basalt. Primary igneous phases have been entirely pseudomorphed by calcic plagioclase+magnesium hornblende+chlorite+titanite+albitized plagioclase+vein epidote and sulfides. Despite the extensive hydrothermal metasomatism, original textures including hyaloclastite glass shards, lithic clasts, chilled margins, and shell-fragment molds are superbly preserved. Multi-collector LA-ICP-MS strontium isotope ratio (87Sr/86Sr) measurements of vein epidote from the core are consistent with seawater as the dominant recharge fluid. Epidote-hosted fluid inclusion homogenization temperature and freezing point depression measurements suggest that the RN-17B core records cooling through the two-phase boundary for seawater over time to current in-situ measured temperatures. Electron microprobe analyses of hydrothermal hornblende and hydrothermal plagioclase confirm that while alteration is of amphibolite-grade, it is in disequilibrium and the extent of alteration is dependent upon protolith type and water/rock ratio. Alteration in the RN-17B core bares many similarities to that of Type II basalts observed in Mid-Atlantic Ridge samples.

KW - Epidote

KW - Geothermal

KW - Hydrothermal alteration

KW - Iceland

KW - RN-17B Drill Core

KW - Reykjanes

UR - http://www.scopus.com/inward/record.url?scp=84933073486&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84933073486&partnerID=8YFLogxK

U2 - 10.1016/j.jvolgeores.2015.06.009

DO - 10.1016/j.jvolgeores.2015.06.009

M3 - Article

AN - SCOPUS:84933073486

VL - 302

SP - 47

EP - 63

JO - Journal of Volcanology and Geothermal Research

JF - Journal of Volcanology and Geothermal Research

SN - 0377-0273

ER -

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

Abstract

Bibliographical note

Keywords

Access

Other files and links

Fingerprint

Cite this