2026-04-30T13:37:54Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:642016-11-25T15:11:58ZDOIDBDOIDB.SDDB

false3DOIDB.SDDB 10.1594/GFZ.SDDB.1121 SAFOD Deutsches GeoForschungsZentrum GFZ 2008 San Andreas Fault-Zone Observatory at Depth Land based Array Induction Four Foot Conductivity A60 Array Induction Four Foot Resistivity A10 Array Induction Four Foot Resistivity A20 Array Induction Four Foot Resistivity A30 Array Induction Four Foot Resistivity A60 Array Induction Four Foot Resistivity A90 Array Induction Mud Resistivity Fully Calibrated Array Induction One Foot Resistivity A10 Array Induction One Foot Resistivity A20 Array Induction One Foot Resistivity A30 Array Induction One Foot Resistivity A60 Array Induction One Foot Resistivity A90 Array Induction One Foot Rt Array Induction One Foot Rxo Array Induction Two Foot Conductivity A60 Array Induction Two Foot Conductivity A90 Array Induction Two Foot Inner Diameter of Invasion Array Induction Two Foot Outer Diameter of Invasion (D2) Array Induction Two Foot Resistivity A10 Array Induction Two Foot Resistivity A20 Array Induction Two Foot Resistivity A30 Array Induction Two Foot Resistivity A60 Array Induction Two Foot Resistivity A90 Array Induction Two Foot Rt Array Induction Two Foot Rxo Backscatter Delta Rho Cable Tension Cal. Caliper calculation Caliper 1 Caliper 2 Cartridge Temperature Computed Gamma Ray Conductivity logging Corrected Far Thermal Counting Rate Corrected Near Thermal Counting Rate Delta Thermal Neutron Porosity Density correction Differential Caliper Enhanced Thermal Neutron Porosity environmentally corrected gamma-ray Formation Potassium Concentration Formation Thorium Concentration Formation Uranium Concentration gamma ray gamma ray logging Generalized Borehole Temperature HGNS HGNS deviation High Resolution Invaded Zone Resistivity HILT HiRes Enhanced Thermal Neutron Porosity HiRes Gamma-Ray HiRes Thermal Neutron Porosity HNGS Hole Azimuth Hole Deviation HRCC HRDD MCFL Memorized Pad 1 Azimuth Memorized relative bearing Micro Inverse Resistivity Micro Normal Resistivity Pad 1Azimuth Photoelectric Factor Correction Porosity CrossPlot Relative Bearing Resistivity logging Sonde deviation SP Armor Return Spontaneous Potential Shifted Standard Gamma Ray Standard Resolution Density Porosity Standard Resolution Density Standoff Standard Resolution Formation Density Standard Resolution Formation Photoelectric Factor Standard Resolution Invaded Zone Resistivity Standard Resolution Resistivity Standoff temperature Thermal Neutron Porosity Thermal Neutron Porosity (Ratio Method) LL3, DIL, DLL 2008-08-27 eng Dataset 106926 DataPoints text/tab-separated-values 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 aseismic creep and repeating microearthquakes. It lies at the extreme northern end of the rupture zone of the 1966, Magnitude 6 Parkfield earthquake, the most recent in a series of events that have ruptured the fault five times since 1857. The Parkfield region is the most comprehensively instrumented section of a fault anywhere in the world, and has been the focus of intensive study for the past two decades. This data set contains open hole geophysical wireline logging data from 1894-2123m (rel. to rig floor, 9,45m abv gnd) 35.9712 -120.5513 35.9713 -120.5512