26 Works

Satellite Problems for Final Science GPS Orbits

Markus Rothacher, Reinhard Dietrich, Peter Steigenberger, Mathias Fritsche & Axel Ruelke
Satellite Problems for Final Science GPS Orbits after Reprocessing usingBernese Software.

SAFOD Main Hole downhole logging data phase 1.2, 2812-3043m

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

Pollen counts from Kasten corer CON01-603-5, CONTINENT Ridge

Dieter Demske, Wojciech Granoszewski & Georg Heumann
Pollen counts from Kasten corer CON01-603-5 at CONTINENT Ridge.

Clay mineralogy and sedimentology of coring Site BDP-1-B (BDP93-2)

Richard Yuretich, Martin Melles, Brenn Sarata & Hannes Grobe
Lake Baikal, in south-central Siberia, has been the focus of an international effort (the Baikal Drilling Project; BDP) to obtain continuous long cores (upwards of 100 m) from this unique rift-valley lake and to interpret the paleoclimatic history from various proxy data. As part of this effort, the clay minerals were examined by two research teams. A consistent clay-mineral assemblage, containing illite, interstratified illite-smectite, chlorite, and kaolinite as the major minerals, characterizes much of the...

SAFOD Main Hole downhole logging data phase 1.1

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 2 (2005), 3387-3799m

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 2 (2005), 2975-3387m

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 1.2, 2583-2812m

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 1.2, 2353-2582m

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 1.2 2124-2353m, year: 2004

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 1.2 1894-2123m, year: 2004

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

SAFOD Main Hole downhole logging data phase 1.2 1932-2041m

SAFOD
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major plate-bounding fault. SAFOD will drill and instrument an inclined borehole across the San Andreas Fault Zone to a depth of 3.2 km, targeting a repeating microearthquake source. The drill site is located west of the vertical San Andreas Fault on a segment of the fault that moves through a combination of...

Magnetic field uplog, 19990705 for HSDP-2-A (592.5 m - 998.5 m)

Martin Leven & Erich Steveling
A quasi-continuous magnetic log has been obtained in the Hawaii Scientific Drilling Project 2 (HSDP-2) between 600 m and 1800 m, which corresponds to a time interval of approximately 350 ka to 480 ka. A tri-axial borehole magnetometer was employed to measure the horizontal and vertical magnetic fields. Measurements were taken in downhole and uphole runs, with a good correlation between the two. In a first step the logs were corrected for the transfer function...

Magnetic field uplog, 19990705 for HSDP-2-A

Martin Leven & Erich Steveling
A quasi-continuous magnetic log has been obtained in the Hawaii Scientific Drilling Project 2 (HSDP-2) between 600 m and 1800 m, which corresponds to a time interval of approximately 350 ka to 480 ka. A tri-axial borehole magnetometer was employed to measure the horizontal and vertical magnetic fields. Measurements were taken in downhole and uphole runs, with a good correlation between the two. In a first step the logs were corrected for the transfer function...

Magnetic field downlog 19990704 for HSDP-2-A

Martin Leven & Erich Steveling
A quasi-continuous magnetic log has been obtained in the Hawaii Scientific Drilling Project 2 (HSDP-2) between 600 m and 1800 m, which corresponds to a time interval of approximately 350 ka to 480 ka. A tri-axial borehole magnetometer was employed to measure the horizontal and vertical magnetic fields. Measurements were taken in downhole and uphole runs, with a good correlation between the two. In a first step the logs were corrected for the transfer function...

Downhole Resistivity log for HSDP-2-A (environmentally corrected)

Arno Buysch, Renate Pechnig, Jürgen Wohlenberg, Jochem Kück & Ulrich Harms
The GFZ Potsdam started a log interpretation study in cooperation with the Technical University of Aachen. As a first result, the logged profile allows for a subdivision of the lithological profile into at least two major zones: (1) a subaerial zone (1900-3600ft) and (2) a submarine zone (3600-6100ft). In addition, the geophysical measurements indicate a further subdivision into the Log Units 1-4 , each unit distinguished by different geophyshical log responses: (Fig.2) (Fig.4) The basaltic...

Downhole Resistivity log for HSDP-2-A

Arno Buysch, Renate Pechnig, Jürgen Wohlenberg, Jochem Kück & Ulrich Harms
The GFZ Potsdam started a log interpretation study in cooperation with the Technical University of Aachen. As a first result, the logged profile allows for a subdivision of the lithological profile into at least two major zones: (1) a subaerial zone (1900-3600ft) and (2) a submarine zone (3600-6100ft). In addition, the geophysical measurements indicate a further subdivision into the Log Units 1-4 , each unit distinguished by different geophyshical log responses: (Fig.2) (Fig.4) The basaltic...

Borehole Temperature of HSDP-2-A on 07/02/1999

Grit Dannowski, Jörg Schrötter, Kemal Erbas, Andrea Förster & Ernst Huenges
The temperature pattern is attributed to a superposition of thermal and hydraulic processes. In the deeper borehole (HSDP-2, depth 3.1 km) detailed temperature monitoring was performed. Temperature measurements reveal two different thermal regimes. The upper part is characterised by cold temperatures and a negative temperature gradient similar to those observed in the shallow pilot borehole. Below 1100 m, increasing temperatures are observed. Different processes, such as topographically driven groundwater flow, ingress of salt water and...

Borehole Temperature of HSDP-2-A on 04/19/1999

Grit Dannowski, Jörg Schrötter, Kemal Erbas, Andrea Förster & Ernst Huenges
The temperature pattern is attributed to a superposition of thermal and hydraulic processes. In the deeper borehole (HSDP-2, depth 3.1 km) detailed temperature monitoring was performed. Temperature measurements reveal two different thermal regimes. The upper part is characterised by cold temperatures and a negative temperature gradient similar to those observed in the shallow pilot borehole. Below 1100 m, increasing temperatures are observed. Different processes, such as topographically driven groundwater flow, ingress of salt water and...

Raw pollen data from the Eemian core CON01-603-2

Wojciech Granoszewski, Dieter Demske, Georg Heumann, Malgorzata Nita & A Andreev
The studied core CON01-603-2 was recovered from the Continent site, Northern Basin from a water depth of 386 m (Fig. 1) (see Charlet et al., 2005-this volume). The analysed sequence (725.5–608 cm) consists of mainly of biogenic, diatomaceous sediments, although the upper part of the sequence between ca. 611–608 cm contains more silt particles and less diatoms than the lower part of the sequence. From a depth of 690 cm upwards the sediments are finely...

TerraSAR-X Attitude Data

Markus Rothacher, Christoph Foerste & Wolfgang Koehler
This data set comprises TerraSAR-X attitude data in terms of quaternions.

Final Science GPS Orbits

Markus Rothacher, Reinhard Dietrich, Peter Steigenberger, Mathias Fritsche & Axel Ruelke
Final GPS Satellite Orbits after Reprocessing (homogenesouly reprocessed withBernese GPS Software by TU Munich and TU Dresden).

Final GPS Earth Rotation Parameters

Markus Rothacher, Reinhard Dietrich, Peter Steigenberger, Mathias Fritsche & Axel Ruelke
Final GPS Earth Rotation Parameters (homogenesouly reprocessed with Bernese GPSSoftware by TU Munich and TU Dresden).

The 2008 database release of the World Stress Map Project

Oliver Heidbach, Mark Tingay, Andreas Barth, John Reinecker, Daniel Kurfess & Birgit Mueller
The World Stress Map (WSM) is the global repository for contemporary tectonic stress data from the Earth's crust. Its uniformity and quality is guaranteed through quality ranking of the data according to international standards and a standardized regime assignment. The WSM merges data which otherwise would be fragmented in separate, often inaccessible archives. It provides the long-term preservation of tectonic stress data from physical loss of data carriers or organizational problems of data storage.

Registration Year

  • 2008
    26

Resource Types

  • Dataset
    24

Data Centers

  • Geoforschungszentrum Potsdam
    26