Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/7882
DC Field | Value | Language |
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dc.contributor.authorall | Paulsen, T.; Department of Geology, University of Wisconsin-Oshkosh, Oshkosh, WI 54901 - USA | en |
dc.contributor.authorall | Millan, C.; School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | en |
dc.contributor.authorall | Pierdominici, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.authorall | Wilson, T.; School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | en |
dc.contributor.authorall | Drew, S.; School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | en |
dc.contributor.authorall | ANDRIL-SMS Science Team; http://andrill.org/projects/sms/team.html | en |
dc.date.accessioned | 2012-03-15T15:25:17Z | en |
dc.date.available | 2012-03-15T15:25:17Z | en |
dc.date.issued | 2009 | en |
dc.identifier.uri | http://hdl.handle.net/2122/7882 | en |
dc.description.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. | en |
dc.language.iso | English | en |
dc.relation.ispartof | Terra Antartica | en |
dc.relation.ispartofseries | 1/15 (2009) | en |
dc.subject | Fractures | en |
dc.subject | Downhole logging | en |
dc.subject | Drillcore | en |
dc.subject | Stress | en |
dc.subject | Antarctica | en |
dc.subject | Drilling | en |
dc.title | Fracture Logging of the AND-2A Core, ANDRILL Southern McMurdo Sound Project, Antarctica | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.description.pagenumber | 69-76 | en |
dc.subject.INGV | 04. Solid Earth::04.02. Exploration geophysics::04.02.05. Downhole, radioactivity, remote sensing, and other methods | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.09. Structural geology | en |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous | en |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.05. Stress | en |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics | en |
dc.relation.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. | en |
dc.description.obiettivoSpecifico | 3.2. Tettonica attiva | en |
dc.description.journalType | N/A or not JCR | en |
dc.description.fulltext | open | en |
dc.contributor.author | Paulsen, T. | en |
dc.contributor.author | Millan, C. | en |
dc.contributor.author | Pierdominici, S. | en |
dc.contributor.author | Wilson, T. | en |
dc.contributor.author | Drew, S. | en |
dc.contributor.author | ANDRIL-SMS Science Team | en |
dc.contributor.department | Department of Geology, University of Wisconsin-Oshkosh, Oshkosh, WI 54901 - USA | en |
dc.contributor.department | School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.department | School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | en |
dc.contributor.department | School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | en |
dc.contributor.department | http://andrill.org/projects/sms/team.html | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Department of Geology, University of Wisconsin Oshkosh, Oshkosh, Wisconsin 54901, USA | - |
crisitem.author.dept | Ohio State University, Department of Geological Sciences, 275 Mendenhall Lab, 125 South Oval Mall, Columbus, Ohio 43210, USA | - |
crisitem.author.dept | Byrd Polar Research Centre, The Ohio State University, Columbus, OH 43210, USA | - |
crisitem.author.dept | School of Earth Sciences, Ohio State University, 125 S. Oval Mall, Columbus, OH 43210 - USA | - |
crisitem.author.dept | 0 | - |
crisitem.author.orcid | 0000-0003-4140-5904 | - |
crisitem.author.orcid | 0000-0002-5368-4536 | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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Paulsen_etal_TerraAnt_2008.pdf | Main article | 1.25 MB | Adobe PDF | View/Open |
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