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Grawinkel, Andrea, Stöckhert, Bernhard (1997) Hydrostatic pore fluid pressure to 9 km depth - Fluid inclusion evidence from the KTB deep drill hole. Geophysical Research Letters, 24 (24) 3273-3276 doi:10.1029/97gl03309

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Reference TypeJournal (article/letter/editorial)
TitleHydrostatic pore fluid pressure to 9 km depth - Fluid inclusion evidence from the KTB deep drill hole
JournalGeophysical Research Letters
AuthorsGrawinkel, AndreaAuthor
Stöckhert, BernhardAuthor
Year1997 (December 15)Volume24
Issue24
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/97gl03309Search in ResearchGate
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Mindat Ref. ID787449Long-form Identifiermindat:1:5:787449:3
GUID0
Full ReferenceGrawinkel, Andrea, Stöckhert, Bernhard (1997) Hydrostatic pore fluid pressure to 9 km depth - Fluid inclusion evidence from the KTB deep drill hole. Geophysical Research Letters, 24 (24) 3273-3276 doi:10.1029/97gl03309
Plain TextGrawinkel, Andrea, Stöckhert, Bernhard (1997) Hydrostatic pore fluid pressure to 9 km depth - Fluid inclusion evidence from the KTB deep drill hole. Geophysical Research Letters, 24 (24) 3273-3276 doi:10.1029/97gl03309
In(1997, December) Geophysical Research Letters Vol. 24 (24) American Geophysical Union (AGU)

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Dresen, Georg, Duyster, Johannes, Stöckhert, Bernhard, Wirth, Richard, Zulauf, Gernold (1997) Quartz dislocation microstructure between 7000 m and 9100 m depth from the Continental Deep Drilling Program KTB. Journal of Geophysical Research: Solid Earth, 102. 18443-18452 doi:10.1029/96jb03394
O'Brien, Patrick J., Duyster, Johannes, Grauert, Borwin, Schreyer, Werner, Stöckhert, Bernhard, Weber, Klaus (1997) Crustal evolution of the KTB drill site: From oldest relics to the Late Hercynian granites. Journal of Geophysical Research: Solid Earth, 102. 18203-18220 doi:10.1029/96jb03397
Haak, Volker, Jones, Alan G. (1997) Introduction to Special Section: The KTB Deep Drill Hole. Journal of Geophysical Research: Solid Earth, 102. 18175-18177 doi:10.1029/96jb03944
Okaya, David (2004) P wave material anisotropy of a tectono-metamorphic terrane: An active source seismic experiment at the KTB super-deep drill hole, southeast Germany. Geophysical Research Letters, 31 (24) doi:10.1029/2004gl020855
Beilecke, Thies (2004) Quantification of seismic scattering in situ with the conversion log method: A study from the KTB super-deep drill hole. Geophysical Research Letters, 31 (16) doi:10.1029/2004gl020100
Coyle, Brian J., Zoback, Mark D. (1988) In situpermeability and fluid pressure measurements at ∼2 km depth in the Cajon Pass research well. Geophysical Research Letters, 15 (9) 1029-1032 doi:10.1029/gl015i009p01029
Zoback, Mark D., Harjes, Hans-Peter (1997) Injection-induced earthquakes and crustal stress at 9 km depth at the KTB deep drilling site, Germany. Journal of Geophysical Research: Solid Earth, 102. 18477-18491 doi:10.1029/96jb02814
Castle, John C., Creager, Kenneth C. (1997) Seismic evidence against a mantle chemical discontinuity near 660 km depth beneath Izu-Bonin. Geophysical Research Letters, 24 (3) 241-244 doi:10.1029/96gl03829
Schleicher, Anja M., Tourscher, Sara N., van der Pluijm, Ben A., Warr, Laurence N. (2009) Constraints on mineralization, fluid‐rock interaction, and mass transfer during faulting at 2–3 km depth from the SAFOD drill hole. Journal of Geophysical Research, 114. doi:10.1029/2008jb006092
Antonioli, Andrea (2005) Fluid flow and seismicity pattern: Evidence from the 1997 Umbria-Marche (central Italy) seismic sequence. Geophysical Research Letters, 32 (10) doi:10.1029/2004gl022256
Huenges, Ernst (1997) Factors controlling the variances of seismic velocity, density, thermal conductivity and heat production of cores from the KTB Pilot Hole. Geophysical Research Letters, 24 (3) 341-344 doi:10.1029/96gl02890
 
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