[HTML][HTML] A review of prokaryotic populations and processes in sub-seafloor sediments, including biosphere: geosphere interactions

RJ Parkes, B Cragg, E Roussel, G Webster… - Marine Geology, 2014 - Elsevier
A general review of the sub-seafloor biosphere is presented. This includes an update and
assessment of prokaryotic cell distributions within marine sediments, current deepest 1922 …

Sixty years of anisotropy of magnetic susceptibility in deformed sedimentary rocks

JM Parés - Frontiers in Earth Science, 2015 - frontiersin.org
The use of the Anisotropy of Magnetic Susceptibility (AMS) has become a rather common
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …

[책][B] Global tectonics

P Kearey, KA Klepeis, FJ Vine - 2009 - books.google.com
The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …

Comparison of smectite-and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts

DM Saffer, C Marone - Earth and Planetary Science Letters, 2003 - Elsevier
Along plate boundary subduction thrusts, the transformation of smectite to illite within fault
gouge at temperatures of∼ 150° C is one of the key mineralogical changes thought to …

[PDF][PDF] Structural and seismic stratigraphic framework of the NanTroSEIZE Stage 1 transect

GF Moore, JO Park, NL Bangs, SP Gulick… - Proc. IODP …, 2009 - researchgate.net
The location of the Integrated Ocean Drilling Program's (IODP) Nankai Trough Seismogenic
Zone Experiment (NanTroSEIZE) was based on regional two-dimensional seismic reflection …

Elevated fluid pressure and extreme mechanical weakness of a plate boundary thrust, Nankai Trough subduction zone

HJ Tobin, DM Saffer - Geology, 2009 - pubs.geoscienceworld.org
Pore fluid pressure is a key parameter governing both the shear strength of faults and the
conditions for seismic and tsunamigenic slip on subduction zone megathrusts. However …

Gas hydrate, fluid flow and free gas: Formation of the bottom-simulating reflector

RR Haacke, GK Westbrook, RD Hyndman - Earth and Planetary Science …, 2007 - Elsevier
Gas hydrate in continental margins is commonly indicated by a prominent bottom-simulating
seismic reflector (BSR) that occurs a few hundred metres below the seabed. The BSR marks …

Compositional and fluid pressure controls on the state of stress on the Nankai subduction thrust: A weak plate boundary

KM Brown, A Kopf, MB Underwood… - Earth and Planetary …, 2003 - Elsevier
We show that both fault mineralogy and regional excess fluid pressure contribute to low
resolved shear stresses on the Nankai subduction plate boundary off southwest Japan. Ring …

Diversity of prokaryotes and methanogenesis in deep subsurface sediments from the Nankai Trough, Ocean Drilling Program Leg 190

CJ Newberry, G Webster, BA Cragg… - Environmental …, 2004 - Wiley Online Library
Summary Diversity of Bacteria and Archaea was studied in deep marine sediments by PCR
amplification and sequence analysis of 16S rRNA and methyl co‐enzyme M reductase …

Broad, weak regions of the Nankai Megathrust and implications for shallow coseismic slip

NLB Bangs, GF Moore, SPS Gulick… - Earth and Planetary …, 2009 - Elsevier
Deep within the Nankai Trough subduction zone the plate-boundary thrust slips along a well-
imaged megasplay fault system during the megathrust earthquakes that regularly strike …