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

SAFOD

2008

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...

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

SAFOD

2008

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...

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

SAFOD

2008

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...

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

SAFOD

2008

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...

SAFOD borehole trajectory data in absolute coordinates (UTM) and in coordinates relative to drilling platform

SAFOD

2007

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...

SAFOD Main Hole downhole logging data phase 1.1

SAFOD

2007

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...

SAFOD Main Hole downhole logging data phase 1.2 1744-1932m

SAFOD

2008

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...

Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data from P-rich samples

Fagel, Natalie | Alleman, Laurent | Granina, L | Hatert, F | Thamo-Boszo, Edit | Cloots, R | André, Luc

2006

The sediment cores were sampled with a resolution of 10 cm, resulting in a total of 290 samples (Table 2). Around 250 mg of dried sediments was mechanically crushed through 100–200-μm mesh then processed by an alkaline digestion (Lithium meta-borate) in a Pt crucible at 1000 °C for 1 h. The...

Age models based on palaeomagnetic measurements for the two cores analysed, CON01-603-2 (Continent Ridge) and VER98-1-14 (Academician Ridge) showing the correlation points to the reference record

Mackay, Anson | Rioual, Patrick

2006

Palaeomagnetism was the method used for dating sediments older than the time span covered by AMS 14C dating. Geomagnetic palaeointensities recorded in Lake Baikal sediments were tuned to a reference curve (the record from ODP Site 984, Channell, 1999) whose chronology is well constrained...

Data concerning preparation of pollen concentrates and graphite targets and results of dating.

Piotrowska, Natalia | Bluszcz, Andrzej | Demske, Dieter | Granoszewski, Wojciech | Heumann, Georg

2006

Laboratory processing of concentrates was aimed at the removal of non-sporomorph organic matter by means of chemical treatment, micro-sieving and heavy liquid seperation. The optained concentrates were checked under the microscope and sample purity was estimated on the basis of particle counts....