Examination of mineral assemblage and chemical composition in the fracture zone of the Nojima Fault at a depth of 1140 m: Analyses of the Hirabayashi NIED drill cores

Island Arc

Volumn 10, Issue 3-4, 2001, Pages 422-429

  Matsuda, Tatsuo ^a   Arai, Takashi ^b   Ikeda, Ryuji ^a   Omura, Kentaro ^a   Kobayashi, Kenta ^c   Sano, Hiroyuki ^d   Sawaguchi, Takashi ^e   Tanaka, Hidemi ^f   Tomita, Tomoaki ^g   Tomida, Naoto ^f   Hirano, Satoshi ^h   Ymazaki, Akiko ^e  

^a NATIONAL RESEARCH INSTITUTE FOR EARTH SCIENCE AND DISASTER PREVENTION   (Japan)

^b SHINSHU UNIVERSITY   (Japan)

^c NIIGATA UNIVERSITY   (Japan)

^d UNIVERSITY OF TOKYO   (Japan)

^e WASEDA UNIVERSITY   (Japan)

^f EHIME UNIVERSITY   (Japan)

^g UNIVERSITY OF TSUKUBA   (Japan)

^h JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

Alternation; Drilling; Fault zone; Hyogo ken Nanbu earthquake; Kobe earthquake; Nojima fault

Indexed keywords

CHEMICAL COMPOSITION; FRACTURE ZONE; KOBE EARTHQUAKE 1995; MINERAL ALTERATION; MINERALOGY;

JAPAN;

EID: 0034756874     PISSN: 10384871     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1440-1738.2001.00340.x     Document Type: Article

References (12)

1. An earthquake mechanism based on rapid sealing of faults
2. Structural and fluid-chemical properties of seismogenic normal faults
3. Fluid-rock interactions in faults of crystalline thrust sheets, Northwestern Wyoming, U.S.A. inferences from fault-related rocks
4. The isocon diagram: A simple solution to Gresens' equation for metasomatic alteration
5. Breakdown of feldspar, volume gain and lateral mass transfer during mylonitization of granitoid in a low metamorphic grade shear zone
6. An outline of the fault zone drilling project by NIED in the vicinity of the 1995 Hyogoken Nanbu earthquake, Japan
7. In situ stress measurements in NIED boreholes in and around the fault zone near the 1995 Hyogo-ken Nanbu earthquake Japan
8. Distribution of fault rocks in the fracture zone of the Nojima Fault at a depth of 1140m: Observations from the Hirabayashi NIED drill core
9. Deep fluid circulation in fault zones
10. Fluid flow and volume loss during mylonitization: An origin for phyllonite in an over-thrust setting, North Carolina, U.S.A
11. Volume loss model for trace-element enrichment in mylonites
12. Mode of occurrence of fault rocks in the drilled cores (GSJ and NIED) penetrating the Nojima Earthquake Fault