86 research outputs found
Accretion, structure and hydrology of intermediate spreading-rate oceanic crust from drillhole experiments and seafloor observations
Downhole measurements recorded in the context of the Ocean Drilling Program in Hole 504B, the deepest hole drilled yet into the oceanic crust, are analyzed in terms of accretion processes of the upper oceanic crust at intermediate spreading-rate. The upper part of the crust is found to support the non steady-state models of crustal accretion developed from seafloor observations (Kappel and Ryan, 1986; Gente, 1987). The continuous and vertical nature of borehole measurements provides stratigraphic and structural data that cannot be obtained solely from seafloor studies and, in turn, these models define a framework to analyze the structural, hydrological, and mineralogical observations made in the hole over the past decade.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/43190/1/11001_2005_Article_BF01204282.pd
Tracing of paleo-shear zones by self-potential data inversion: case studies from the KTB, Rittsteig, and Grossensees graphite-bearing fault planes
Vorkommen und Entstehung von tri-oktaedrischen Smektiten in den Basalten und Böden der König-Georg-Insel (S-Shetlands/West-Antarktis)
The Oxygen Isotope Composition of Hercynian Granites and Pre-Hercynian Gneisses from the Schwarzwald, S W Germany
Philosophie und Mathematik - Neue Anschlussmöglichkeiten
Wilholt T. Philosophie und Mathematik - Neue Anschlussmöglichkeiten. In: Emmermann R, Altenbach H-J, eds. An den Fronten der Forschung: Kosmos, Erde, Leben; Verhandlungen der Gesellschaft Deutscher Naturforscher und Ärzte, 122. Versammlung, 21.-24. September 2002, Halle/Saal. Verhandlungen der Gesellschaft Deutscher Naturforscher und Ärzte. Vol 122. Stuttgart: Hirzel; 2003: 287-291
PMD12 Economic Impact analysis of Sterilization of Rigid Endoscopes with Sterradtm versus Steam in Spain
Palaeomagnetism, K-Ar dating and geodynamic setting of igneous rocks in western and central Neuschwabenland, Antarctica
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