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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7882
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dc.contributor.authorallPaulsen, T.; Department of Geology, University of Wisconsin-Oshkosh, Oshkosh, WI 54901 - USAen
dc.contributor.authorallMillan, C.; School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USAen
dc.contributor.authorallPierdominici, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallWilson, T.; School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USAen
dc.contributor.authorallDrew, S.; School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USAen
dc.contributor.authorallANDRIL-SMS Science Team; http://andrill.org/projects/sms/team.htmlen
dc.date.accessioned2012-03-15T15:25:17Zen
dc.date.available2012-03-15T15:25:17Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/7882en
dc.description.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.en
dc.language.isoEnglishen
dc.relation.ispartofTerra Antarticaen
dc.relation.ispartofseries1/15 (2009)en
dc.subjectFracturesen
dc.subjectDownhole loggingen
dc.subjectDrillcoreen
dc.subjectStressen
dc.subjectAntarcticaen
dc.subjectDrillingen
dc.titleFracture Logging of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarcticaen
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber69-76en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.05. Downhole, radioactivity, remote sensing, and other methodsen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.05. Stressen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.relation.referencesLi 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.en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextopenen
dc.contributor.authorPaulsen, T.en
dc.contributor.authorMillan, C.en
dc.contributor.authorPierdominici, S.en
dc.contributor.authorWilson, T.en
dc.contributor.authorDrew, S.en
dc.contributor.authorANDRIL-SMS Science Teamen
dc.contributor.departmentDepartment of Geology, University of Wisconsin-Oshkosh, Oshkosh, WI 54901 - USAen
dc.contributor.departmentSchool of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentSchool of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USAen
dc.contributor.departmentSchool of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USAen
dc.contributor.departmenthttp://andrill.org/projects/sms/team.htmlen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Geology, University of Wisconsin Oshkosh, Oshkosh, Wisconsin 54901, USA-
crisitem.author.deptOhio State University, Department of Geological Sciences, 275 Mendenhall Lab, 125 South Oval Mall, Columbus, Ohio 43210, USA-
crisitem.author.deptByrd Polar Research Centre, The Ohio State University, Columbus, OH 43210, USA-
crisitem.author.deptSchool of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA-
crisitem.author.dept0-
crisitem.author.orcid0000-0003-4140-5904-
crisitem.author.orcid0000-0002-5368-4536-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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