Late-interseismic state of a continental plate-bounding fault: Petrophysical results from DFDP-1 wireline logging and core analysis, Alpine Fault, New Zealand

Publikationstyp:
Zeitschriftenaufsatz
Metadaten:
Autoren
  • J Townend
  • R Sutherland
  • VG Toy
  • JD Eccles
  • C Boulton
  • SC Cox
  • D McNamara
Autoren-URL
https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=fis-test-1&SrcAuth=WosAPI&KeyUT=WOS:000326247700029&DestLinkType=FullRecord&DestApp=WOS_CPL
DOI
10.1002/ggge.20236
Externe Identifier
  • Clarivate Analytics Document Solution ID: 242MZ
ISSN
1525-2027
Ausgabe der Veröffentlichung
9
Zeitschrift
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Schlüsselwörter
  • Alpine Fault
  • DFDP-1
  • fault zone structure
  • earthquake cycle
  • principal component analysis
  • wireline logging
Paginierung
3801 - 3820
Datum der Veröffentlichung
2013
Status
Published
Titel
Late-interseismic state of a continental plate-bounding fault: Petrophysical results from DFDP-1 wireline logging and core analysis, Alpine Fault, New Zealand
Sub types
  • Article
Ausgabe der Zeitschrift
14

Datenquelle: Web of Science (Lite)

Andere Metadatenquellen:
Abstract
<jats:p>We present a geophysical characterization at 0.1–100 m scales of a major plate‐bounding continental fault in a late‐interseismic state. The Alpine Fault produces M<jats:sub>W</jats:sub>∼8 earthquakes every 200–400 years and last ruptured in 1717 AD. Wireline geophysical logs and rock cores extending from one side of the Alpine Fault to the other were acquired in two boreholes drilled in 2011 at Gaunt Creek during the first phase of the Deep Fault Drilling Project (DFDP‐1). These data document ambient conditions under which the next Alpine Fault earthquake will occur. Principal component analysis of the wireline logging data reveals that &gt;80% of the variance is accounted for by electrical, acoustic, and natural gamma properties, and preliminary multivariate classification enables the lithologies of sections of missing core to be reconstructed from geophysical measurements. The fault zone exhibits systematic variations in properties consistent with common processes of progressive alteration and comminution near the principal slip zone, superimposed on different protolith compositions. Our observations imply that the fault zone has the opposite sense of elastic asymmetry at 0.1–100 m scales to that of the crustal‐scale orogen imaged by remote geophysical methods. On the basis of the fault‐zone scale asymmetry, the bimaterial interface model of preferred earthquake rupture directions implies a northeastward direction of preferred Alpine Fault rupture. On‐going characterization of the structural and hydraulic architecture of the Alpine Fault will improve our understanding of the relationship between in situ conditions, earthquake rupture processes, and the hazards posed by future earthquakes.</jats:p>
Autoren
  • J Townend
  • R Sutherland
  • VG Toy
  • JD Eccles
  • C Boulton
  • SC Cox
  • D McNamara
DOI
10.1002/ggge.20236
eISSN
1525-2027
ISSN
1525-2027
Ausgabe der Veröffentlichung
9
Zeitschrift
Geochemistry, Geophysics, Geosystems
Sprache
en
Online publication date
2013
Paginierung
3801 - 3820
Datum der Veröffentlichung
2013
Status
Published
Herausgeber
American Geophysical Union (AGU)
Herausgeber URL
http://dx.doi.org/10.1002/ggge.20236
Datum der Datenerfassung
2023
Titel
Late‐interseismic state of a continental plate‐bounding fault: Petrophysical results from DFDP‐1 wireline logging and core analysis, Alpine Fault, New Zealand
Ausgabe der Zeitschrift
14

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