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(Table 1) Orientation of coring during ODP Leg 115
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(Table 3) Triaxial test results of ODP Leg 112 samples
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(Table 1) Paleomagnetic orientation of ODP Hole 107-651A peridotites
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(Table T15) Principal component analysis results from U-channel paleomagnetic...
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(Table T14) Principal component analysis results from U-channel paleomagnetic...
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(Table T13) Principal component analysis results from U-channel paleomagnetic...
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(Table T12) Principal component analysis results from U-channel paleomagnetic...
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(Table T11) Principal component analysis results from U-channel paleomagnetic...
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(Table T10) Principal component analysis results from U-channel paleomagnetic...
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(Table 1) Description of structures in cores at DSDP Holes 59-451, 59-448A an...
Fifteen lengths of Leg 59 cores (primarily from Hole 451 as well as from Holes 447A and 448A) exhibiting macroscopic faults were selected by Dr. R. B. Scott (Co-Chief Scientist,... -
(Table 1) Anisotropy of magnetic susceptibility of basalts at DSDP Hole 89-462A
Measurements of the anisotropy of magnetic susceptibility (AMS) in basalts cored from 1070 to 1209 m sub-bottom depth in Hole 462A reveal that samples with a high ratio of... -
(Table 1) Paleomagnetic of reoriented core pieces of IODP Hole 304-U1309D
Oceanic core complexes expose lower crustal and upper mantle rocks on the seafloor by tectonic unroofing in the footwalls of large-slip detachment faults. The common occurrence... -
(Table 3) Main results of the stress tensor inversion of selected populations...
Drilling at Site 808 (ODP Leg 131) provided an extensive record of the discrete brittle structures (small faults and shear bands) at the toe of the Nankai accretionary complex.... -
(Table T1) Gas hydrate fabric and dipping angles of ODP Leg 204 sediments
The sediments of Hydrate Ridge/Cascadia margin contain extensive amounts of gas hydrate. A total of 57 sediment samples including gas hydrate were preserved in liquid nitrogen... -
(Table 1) Sample identifier, fabric and dipping angle from ODP Leg 204 sample...
Drilling on Hydrate Ridge, offshore Oregon, during ODP Leg 204 enabled us to investigate fabrics of gas hydrate samples in a wide depth range of the gas hydrate stability zone... -
Paleointensity of various DSDP sites (Table 3)
The existing database for paleointensity estimates of the ancient geomagnetic field contains more than 1500 data points collected through decades of effort. Despite the huge... -
Morphometric redefinition of the component chronospecies of the Globorotalia ...
Phylo-zonations (or lineage-zonations) are based upon morphological changes within individual evolutionary lineages. These zonations, although potentially of use for... -
Seawater carbonate chemistry and effects of ocean acidification and wariming ...
Ocean acidification and warming (OAW) are pressing contemporary issues affecting marine life and specifically calcifying organisms. Here, we investigated the direct effects of... -
Seawater carbonate chemistry and development and growth in early‑stage larvae...
Under the ocean acidification (OA) conditions predicted for 2100, the larval stages of temperate sea urchins are smaller, with reduced and abnormal skeleton and changes in... -
Seawater carbonate chemistry and swimming performance of Tritia reticulata (L...
Tritia reticulata (L.) is a neogastropod ubiquitous in the coastal communities of the NE Atlantic. Its life cycle relies on the swimming performance of planktonic early life...
