Geochemical bias in drill cutting samples versus drill core samples returned from the Reykjanes Geothermal System, Iceland

Fowler, Andrew P. G.; Zierenberg, Robert A.

doi:10.1016/j.geothermics.2016.02.007

Title: Geochemical bias in drill cutting samples versus drill core samples returned from the Reykjanes Geothermal System, Iceland

Full Record
Other Related Research

Authors:

; Zierenberg, Robert A.

Publication Date:: Fri Jul 01 00:00:00 EDT 2016

Sponsoring Org.:: USDOE

OSTI Identifier:: 1348252

Grant/Contract Number:: EE00006748

Resource Type:: Publisher's Accepted Manuscript

Journal Name:: Geothermics

Additional Journal Information:: Journal Name: Geothermics Journal Volume: 62 Journal Issue: C; Journal ID: ISSN 0375-6505

Publisher:: Elsevier

Country of Publication:: United Kingdom

Language:: English

Citation Formats


                    Fowler, Andrew P. G., and Zierenberg, Robert A. Geochemical bias in drill cutting samples versus drill core samples returned from the Reykjanes Geothermal System, Iceland.  United Kingdom: N. p., 2016. 
Web.  doi:10.1016/j.geothermics.2016.02.007.

Copy to clipboard


                    Fowler, Andrew P. G., & Zierenberg, Robert A. Geochemical bias in drill cutting samples versus drill core samples returned from the Reykjanes Geothermal System, Iceland.  United Kingdom.  https://doi.org/10.1016/j.geothermics.2016.02.007

Copy to clipboard


                    Fowler, Andrew P. G., and Zierenberg, Robert A. Fri .  
"Geochemical bias in drill cutting samples versus drill core samples returned from the Reykjanes Geothermal System, Iceland".  United Kingdom.  https://doi.org/10.1016/j.geothermics.2016.02.007.

Copy to clipboard


                    
@article{osti_1348252,

  title        = {Geochemical bias in drill cutting samples versus drill core samples returned from the Reykjanes Geothermal System, Iceland},

  author       = {Fowler, Andrew P. G. and Zierenberg, Robert A.},

  abstractNote = {},

  doi          = {10.1016/j.geothermics.2016.02.007},

  journal      = {Geothermics},

  number       = C,

  volume       = 62,

  place        = {United Kingdom},

  year         = {Fri Jul 01 00:00:00 EDT 2016},

  month        = {Fri Jul 01 00:00:00 EDT 2016}

}

Copy to clipboard

Journal Article:

Free Publicly Available Full Text

Accepted Manuscript (Publisher)

Publisher's Version of Record
https://doi.org/10.1016/j.geothermics.2016.02.007

Other availability

Search WorldCat to find libraries that may hold this journal

Citation Metrics:

Cited by: 7 works

Citation information provided by
Web of Science

Save / Share:

Export Metadata

Save to My Library

Similar Records in DOE PAGES and OSTI.GOV collections:

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

Journal Article Fowler, Andrew P.G. ; Zierenberg, Robert A. ; Schiffman, Peter ; ... - Journal of Volcanology and Geothermal Research

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 techniquesmore »« less
https://doi.org/10.1016/j.jvolgeores.2015.06.009

Full Text Available
Drill cutting and core major, trace and rare earth element anlayses from wells RN-17B and RN-30, Reykjanes, Iceland

Dataset Fowler, Andrew

Analytical results for x-ray fluorescence (XRF) and Inductively Couple Plasma Mass Spectrometry (ICP-MS) measurement of major, trace and rare earth elements in drill cuttings from geothermal wells in Reykjanes, Iceland. Total Fe was analyzed as FeO, therefore is not included under the Fe2O3 column.
https://doi.org/10.15121/1261973

View Dataset
Drill core major, trace and rare earth element anlayses from wells RN-17B and RN-30, Reykjanes, Iceland

Dataset Fowler, Andrew

Analytical results for X-ray fluorescence (XRF) and inductively coupled plasma mass spectrometry (ICP-MS) measurement of major, trace and rare earth elements in drill core from geothermal wells in Reykjanes, Iceland. Total Fe was analyzed as FeO, therefore is not included under the Fe2O3 column.
https://doi.org/10.15121/1261974

View Dataset
Fluid rare earth element anlayses from geothermal wells located on the Reykjanes Peninsula, Iceland and Middle Valley seafloor hydrothermal system on the Juan de Fuca Ridge.

Dataset Fowler, Andrew

Results for fluid rare earth element analyses from four Reykjanes peninsula high-temperature geothermal fields. Data for fluids from hydrothermal vents located 2400 m below sea level from Middle Valley on the Juan de Fuca Ridge are also included. Data have been corrected for flashing. Samples preconcentrated using a chelating resin with IDA functional group (InertSep ME-1). Analyzed using an Element magnetic sector inductively coupled plasma mass spectrometry (ICP-MS).
https://doi.org/10.15121/1261975

View Dataset
Mineral-fluid interaction in the Reykjanes and Svartsengi geothermal systems, Iceland

Journal Article Lonker, S W ; Franzson, H ; Kristmannsdottir, H

Physical observations on features such as temperature, pressure, and formation permeability are integrated with alteration intensity, fluid and secondary mineral compositions, and textures to show the most important thermal, chemical, hydrodynamic, and kinetics factors that control the evolution of two Icelandic geothermal systems, the Reykjanes and Svartsengi systems. There is an increase in alteration intensity and the abundance of fracture and vesicle fillings, a decrease in the abundance of primary minerals, and more extensive compositional heterogeneity near many aquifers, which are defined by circulation losses and temperature and pressure profiles. Features such as resorption and overgrowth textures, absence of systematicmore »« less
https://doi.org/10.2475/ajs.293.7.605

Similar Records