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

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

Rioual, Patrick | Mackay, Anson

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...

Selected electron-microprobe analyses of vivianite and santabarbaraite from Lake Baikal

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

2006

Electron-microprobe analyses (Table 5) were completed on a selection of grains from 11 samples, with a CAMECA SX-50 instrument (University of Louvain-la-Neuve, Belgium), under an accelerating voltage of 15 kV and a probe current of 20 nA. The standards used were the Kabira graftonite (Fe, Mn,...

SAFOD Main Hole downhole logging data phase 1.2 1368-1556m

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 1556-1744m

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 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...

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...

Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis

Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi

2006

Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis (magnetite dissolution and/or greigite formation) and correlation to the relative paleointensity record from ODP Site 984 (Channell, 1999). In addition to AMS 14C dating and the...