Stable isotope constraints on vein formation and fluid evolution along a recent thrust fault in the Cascadia accretionary wedge

Research output: Contribution to journalArticle

10 Citations (Scopus)

Abstract

In situ secondary ionization mass spectrometry (SIMS) analyses of oxygen isotopes in authigenic calcite veins were obtained from an active thrust fault system drilled at Ocean Drilling Program (ODP) Site 892 (44°40.4'N, 125°07.1'W) along the Cascadia subduction margin. The average δ18OPDB value of all samples is -9.9% and the values are the lowest of any measured in active accretionary prisms. Ranges in individual veins can be as much as 19.6%. There is an isotopic stratigraphy related to the structural stratigraphy. Mean isotope values in the hanging wall, thrust, and footwall are -14.4%, -9.5%, and -5.2%, respectively. Several veins and crosscutting vein sequences show a general trend from lower to higher δ18O values over time. Isotopic and textural data indicate several veins formed by a crack-seal mechanism and growth into open fractures. The best explanation for the strong 18O depletions is periodic rapid flow from 2-3km deeper in the prism. Relatively narrow isotopic ranges for most veins suggest that fluids were derived from a similar source depth for each episode of fluid pulse and calcite crystallization. Structural and mass balance considerations are consistent with a record preserved in the veins of ten to hundreds of thousands of years. The fluid pulses may relate to periodic large earthquake events such as those recognized in the paleoseismicity records from the Cascadia margin.

Original languageEnglish (US)
Pages (from-to)300-312
Number of pages13
JournalEarth and Planetary Science Letters
Volume293
Issue number3-4
DOIs
StatePublished - May 2010

Fingerprint

accretionary prism
thrust fault
veins
Isotopes
wedges
Stratigraphy
stable isotope
Calcium Carbonate
isotopes
Prisms
Fluids
fluid
fluids
stratigraphy
Oxygen Isotopes
calcite
paleoseismicity
earthquake event
hanging wall
footwall

Keywords

  • Carbonate
  • Cascadia subduction zone
  • Fluid flow
  • Geochemistry
  • Ocean Drilling Program
  • Oxygen isotopes
  • SIMS
  • Veins

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

@article{64aaa2b9c53a484ea212f10e63546ecd,
title = "Stable isotope constraints on vein formation and fluid evolution along a recent thrust fault in the Cascadia accretionary wedge",
abstract = "In situ secondary ionization mass spectrometry (SIMS) analyses of oxygen isotopes in authigenic calcite veins were obtained from an active thrust fault system drilled at Ocean Drilling Program (ODP) Site 892 (44°40.4'N, 125°07.1'W) along the Cascadia subduction margin. The average δ18OPDB value of all samples is -9.9{\%} and the values are the lowest of any measured in active accretionary prisms. Ranges in individual veins can be as much as 19.6{\%}. There is an isotopic stratigraphy related to the structural stratigraphy. Mean isotope values in the hanging wall, thrust, and footwall are -14.4{\%}, -9.5{\%}, and -5.2{\%}, respectively. Several veins and crosscutting vein sequences show a general trend from lower to higher δ18O values over time. Isotopic and textural data indicate several veins formed by a crack-seal mechanism and growth into open fractures. The best explanation for the strong 18O depletions is periodic rapid flow from 2-3km deeper in the prism. Relatively narrow isotopic ranges for most veins suggest that fluids were derived from a similar source depth for each episode of fluid pulse and calcite crystallization. Structural and mass balance considerations are consistent with a record preserved in the veins of ten to hundreds of thousands of years. The fluid pulses may relate to periodic large earthquake events such as those recognized in the paleoseismicity records from the Cascadia margin.",
keywords = "Carbonate, Cascadia subduction zone, Fluid flow, Geochemistry, Ocean Drilling Program, Oxygen isotopes, SIMS, Veins",
author = "Sample, {James C}",
year = "2010",
month = "5",
doi = "10.1016/j.epsl.2010.02.044",
language = "English (US)",
volume = "293",
pages = "300--312",
journal = "Earth and Planetary Sciences Letters",
issn = "0012-821X",
publisher = "Elsevier",
number = "3-4",

}

TY - JOUR

T1 - Stable isotope constraints on vein formation and fluid evolution along a recent thrust fault in the Cascadia accretionary wedge

AU - Sample, James C

PY - 2010/5

Y1 - 2010/5

N2 - In situ secondary ionization mass spectrometry (SIMS) analyses of oxygen isotopes in authigenic calcite veins were obtained from an active thrust fault system drilled at Ocean Drilling Program (ODP) Site 892 (44°40.4'N, 125°07.1'W) along the Cascadia subduction margin. The average δ18OPDB value of all samples is -9.9% and the values are the lowest of any measured in active accretionary prisms. Ranges in individual veins can be as much as 19.6%. There is an isotopic stratigraphy related to the structural stratigraphy. Mean isotope values in the hanging wall, thrust, and footwall are -14.4%, -9.5%, and -5.2%, respectively. Several veins and crosscutting vein sequences show a general trend from lower to higher δ18O values over time. Isotopic and textural data indicate several veins formed by a crack-seal mechanism and growth into open fractures. The best explanation for the strong 18O depletions is periodic rapid flow from 2-3km deeper in the prism. Relatively narrow isotopic ranges for most veins suggest that fluids were derived from a similar source depth for each episode of fluid pulse and calcite crystallization. Structural and mass balance considerations are consistent with a record preserved in the veins of ten to hundreds of thousands of years. The fluid pulses may relate to periodic large earthquake events such as those recognized in the paleoseismicity records from the Cascadia margin.

AB - In situ secondary ionization mass spectrometry (SIMS) analyses of oxygen isotopes in authigenic calcite veins were obtained from an active thrust fault system drilled at Ocean Drilling Program (ODP) Site 892 (44°40.4'N, 125°07.1'W) along the Cascadia subduction margin. The average δ18OPDB value of all samples is -9.9% and the values are the lowest of any measured in active accretionary prisms. Ranges in individual veins can be as much as 19.6%. There is an isotopic stratigraphy related to the structural stratigraphy. Mean isotope values in the hanging wall, thrust, and footwall are -14.4%, -9.5%, and -5.2%, respectively. Several veins and crosscutting vein sequences show a general trend from lower to higher δ18O values over time. Isotopic and textural data indicate several veins formed by a crack-seal mechanism and growth into open fractures. The best explanation for the strong 18O depletions is periodic rapid flow from 2-3km deeper in the prism. Relatively narrow isotopic ranges for most veins suggest that fluids were derived from a similar source depth for each episode of fluid pulse and calcite crystallization. Structural and mass balance considerations are consistent with a record preserved in the veins of ten to hundreds of thousands of years. The fluid pulses may relate to periodic large earthquake events such as those recognized in the paleoseismicity records from the Cascadia margin.

KW - Carbonate

KW - Cascadia subduction zone

KW - Fluid flow

KW - Geochemistry

KW - Ocean Drilling Program

KW - Oxygen isotopes

KW - SIMS

KW - Veins

UR - http://www.scopus.com/inward/record.url?scp=77951294646&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=77951294646&partnerID=8YFLogxK

U2 - 10.1016/j.epsl.2010.02.044

DO - 10.1016/j.epsl.2010.02.044

M3 - Article

VL - 293

SP - 300

EP - 312

JO - Earth and Planetary Sciences Letters

JF - Earth and Planetary Sciences Letters

SN - 0012-821X

IS - 3-4

ER -