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  5. Fracture Logging of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarctica
 
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Fracture Logging of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarctica

Author(s)
Paulsen, T.  
Department of Geology, University of Wisconsin-Oshkosh, Oshkosh, WI 54901 - USA  
Millan, C.  
School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA  
Pierdominici, S.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Wilson, T.  
School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA  
Drew, S.  
School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA  
ANDRIL-SMS Science Team
http://andrill.org/projects/sms/team.html  
Language
English
Obiettivo Specifico
3.2. Tettonica attiva
Status
Published
JCR Journal
N/A or not JCR
Journal
Terra Antartica  
Issue/vol(year)
1/15 (2009)
Pages (printed)
69-76
Date Issued
2009
URI
https://www.earth-prints.org/handle/2122/7882
Subjects
04. Solid Earth::04.02. Exploration geophysics::04.02.05. Downhole, radioactivity, remote sensing, and other methods  
04. Solid Earth::04.04. Geology::04.04.09. Structural geology  
04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous  
04. Solid Earth::04.07. Tectonophysics::04.07.05. Stress  
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics  
Subjects

Fractures

Downhole logging

Drillcore

Stress

Antarctica

Drilling

Abstract
Fractures in AND-2A drillcore were documented in this study. Over 4100 fractures of all
types were logged. A population of 510 steeply-dipping, petal, petal-centreline and core-edge induced
fractures is present, reaching a maximum density of c. 10 fractures/metre. Subhorizontal induced
extension fractures are also abundant. There are 1008 natural fractures in the core, including faults,
brecciated zones, veins and sedimentary intrusions. Kinematic indicators document dominant normal
faulting, although reverse faults are also present. The natural fractures occur in strata ranging in age
from the Miocene to the Plio-Pleistocene.
References
Li Y. & Schmitt D., 1997. Well-bore bottom stress concentration and induced core fractures. American Association of Petroleum
Geologists, Bulletin, 81, 1909-1925.
Lorenz J.C., Finely S.J. & Warpinski N.R., 1990. Significance of coring induced fractures in the Mesaverde core, northwestern
Colorado. American Association of Petroleum Geologists,Bulletin, 74, 1017-1029.
Paulsen T.S., Jarrard R.D., & Wilson T.J., 2002. A simple method for orienting drill core by correlating features in whole-core
scans and oriented borehole wall imagery. Journal of Structural Geology, 24, 1233-1238.
Wilson T., Paulsen T., Läufer A., Millan C., & the ANDRILL-MIS Science Team, 2007. Fracture logging of the AND-1B Core,
McMurdo Ice Shelf Project, Antarctica. Terra Antartica, 14, 175-184.
Type
article
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