Magnetic inference of in situ open microcracks in sandstone samples from the Taiwan Chelungpu Fault Drilling Project (TCDP)

► We investigate the magnetic signature of microcracks in TCDP sandstone. ► Anisotropy of anhysteretic remanent magnetization reflects magnetite neocrystallizations into microcracks network. ► Microcracks in TCDP sandstone are open at depth. This paper presents a thorough magnetic study of centimete...

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Bibliographic Details
Published in:Journal of Asian earth sciences Vol. 45; pp. 179 - 189
Main Authors: Humbert, Fabien, Robion, Philippe, Louis, Laurent, Bartier, Danièle, Ledésert, Béatrice, Song, Sheng-Rong
Format: Journal Article
Language:English
Published: Elsevier Ltd 02-02-2012
Elsevier
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Summary:► We investigate the magnetic signature of microcracks in TCDP sandstone. ► Anisotropy of anhysteretic remanent magnetization reflects magnetite neocrystallizations into microcracks network. ► Microcracks in TCDP sandstone are open at depth. This paper presents a thorough magnetic study of centimeter-sized rock samples from Hole B of the Taiwan Chelungpu Fault Drilling Project (TCDP). Fabrics were obtained from magnetic susceptibility and anhysteretic remanent magnetization are interpreted using whole rock and magnetic mineralogy characterization. We infer the presence in the sandstone lithology of secondary magnetite coating a dense network of microcracks. Using other evidence from ferrofluid saturation experiments, we conclude that this network of microcracks is not sealed but open in situ, and should therefore be incorporated in the interpretation of seismic and borehole scale studies in the TCDP area.
ISSN:1367-9120
1878-5786
DOI:10.1016/j.jseaes.2011.10.009