![integrated age of water integrated age of water](https://s3.wp.wsu.edu/uploads/sites/1125/2020/04/14_HydroTablePNG-396x223.png)
NRM, magnetic susceptibility, and Königsberger ratioĭownhole variations of paleomagnetic data obtained from Hole C0012A are shown in Figure F35. Additional postcruise measurements with a cryogenic magnetometer at Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, made it possible to characterize the remanent magnetization of basaltic samples collected for shipboard study. Because of a malfunction of the spinner magnetometer toward the end of the expedition, only two samples from basaltic basement yielded measurements of remanent magnetization on board the ship. The Königsberger ( Q) ratio was also determined for all measured samples. Volume magnetic susceptibility of these discrete samples was measured after AF demagnetization with the Kappabridge KLY 35, except for 96 discrete samples from Cores 322-C0012A-4R through 20R, which were measured for anisotropy of magnetic susceptibility (AMS) with the Kappabridge KLY 35 before the AF demagnetization experiments.
![integrated age of water integrated age of water](https://www.tetonscience.org/wp-content/uploads/2019/07/IMG_2128-e1563471398869.jpg)
We analyzed the results in Zijderveld diagrams (Zijderveld, 1967) and calculated the characteristic remanent magnetization (ChRM) direction using principal component analysis (Kirschvink, 1980). We completed natural remanent magnetization (NRM) measurements and alternating-field (AF) demagnetization on a total of 269 discrete samples from Hole C0012A. Sample depth and type distribution.ĭoi:10.2204/iodp.proc.322.104.2010 Paleomagnetism Estimated major ion concentration at pore fluid anomaly. Paleomagnetic directions for reorientation of coherent blocks. Model A paleomagnetic and biostratigraphic age datums. Planktonic foraminifer events and absolute age. Calcareous nannofossil events and absolute age. Model B paleomagnetic and biostratigraphic age datums. Stratigraphic relations correlated to units in ODP and IODP sites. 3-D PSDM seismic reflection profile, Cross-line 435. H 2 concentrations in sediment samples as a function of time. Inorganic carbon, TOC, TN, and total sulfur. Sulfate distribution compared with ODP Leg 190 Sites. Interstitial water volume recovered from whole-round sections. Electrical resistivity and vertical-plane anisotropy for discrete cube samples. P-wave velocity versus porosity for discrete samples. P-wave velocity and horizontal and vertical-plane anisotropy on discrete cube samples. Undrained shear strength in the shallow section. MAD results, discrete mud(stone) and sand(stone) samples. Vector endpoint diagrams of magnetization directions, basement basaltic rocks. Vector endpoint diagrams of magnetization. Paleomagnetic measurements on discrete samples. Sedimentation rates based on calcareous nannofossils.
![integrated age of water integrated age of water](https://i1.rgstatic.net/publication/332767892_Impacts_of_soil_and_water_conservation_practices_on_soil_property_and_wheat_productivity_in_Southern_Ethiopia/links/5cc90c1ca6fdcc1d49bc14e2/largepreview.png)
Chronostratigraphic correlation based on calcareous nannofossils and planktonic foraminifers. Sheath folding in laminated volcaniclastic sandstone. Mineral-filling vein and layer-parallel veins. Stereo plots of bedding plane and faults after paleomagnetic correction. Dip angle variation of bedding and fault planes. 3-D PSDM seismic reflection profile, In-line 95. Photographs of different alteration types. Photomicrographs and close-up photographs of altered basalts. Photomicrographs of different alteration types. Close-up photographs of heterogeneous basalt pieces. Close-up photographs of basement material. Red calcareous claystone overlying basalt basement. Smear slide data for sandstones of Unit V. Laminated volcaniclastic siltstone sandstone. Logging and core-log-seismic integration.Characterization of the type and maturity of organic matter by Rock-Eval pyrolysis.Carbon, nitrogen, and sulfur contents of the solid phase.Chemical changes due to alteration of volcaniclastics.Comparison with Site C0011 and Sites 11.
![integrated age of water integrated age of water](https://i.pinimg.com/736x/da/33/ea/da33eae5355d979e03ccbbccb7cf5850.jpg)
Anisotropy of P-wave velocity and electrical resistivity.Paleomagnetic characterization of basement rocks.Paleomagnetic reorientation of the cores.Integrated age model and sediment accumulation rates.Polarity sequence and magnetostratigraphy.NRM, magnetic susceptibility, and Königsberger ratio.Sedimentation rates based on biostratigraphy.Comparison between Site C0012 and ODP/IODP sites.Paleogeography and sediment provenance at Site C0012.Sediment accumulation rates at Site C0012.Lithologic Unit VII (Kashinosaki Knoll basement).Lithologic Unit V (volcaniclastic-rich).Lithologic Unit IV (lower Shikoku Basin turbidites).Lithologic Unit III (lower Shikoku Basin hemipelagites).Lithologic Unit II (middle Shikoku Basin).Lithologic Unit I (upper Shikoku Basin).