Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7882
AuthorsPaulsen, T.* 
Millan, C.* 
Pierdominici, S.* 
Wilson, T.* 
Drew, S.* 
ANDRIL-SMS Science Team* 
TitleFracture Logging of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarctica
Issue Date2009
Series/Report no.1/15 (2009)
URIhttp://hdl.handle.net/2122/7882
KeywordsFractures
Downhole logging
Drillcore
Stress
Antarctica
Drilling
Subject Classification04. 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 
AbstractFractures 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.
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