• THE ORIGIN OF THE OBSERVED LOW-FREQUENCY ELECTRICAL POLARIZATION IN SANDSTONES 

  Scott J.B.T. (2006)

  There has been an increasing debate regarding the mechanism controlling the low-frequency polarization (megahertz to kilohertz) in sandstones. The polarization and related electrical relaxation are extremely important ...
• PORE GEOMETRY OF PERMO-TRIASSIC SANDSTONE FROM MEASUREMENTS OF ELECTRICAL SPECTROSCOPY 

  Scott J.B.T.; Barker R.D. (2006)

  In order to provide an indirect method of estimating the hydraulic properties of sandstone aquifer rocks, electrical spectroscopy measurements were made on Permo-Triassic Sandstone over the frequency range 0.0001-1000 Hz. ...
• CORALS OF THE K/T-BOUNDARY: SCLERACTINIAN CORALS OF THE SUBORDERS ASTROCOENIINA, FAVIINA, RHIPIDOGYRINA AND AMPHIASTRAEINA 

  Baron-Szabo R.C. (2006)

  This taxonomic review of the scleractinian corals of the Maastrichtian and Paleocene period focuses on the scleractinian suborders Astrocoeniina, Faviina, Rhipidogyrina and Amphiastraeina. This, the first extensive compilation ...
• DETERMINING CAPILLARY-PRESSURE CURVE, PORE-SIZE DISTRIBUTION, AND PERMEABILITY FROM INDUCED POLARIZATION OF SHALEY SAND 

  Tong M.; Wang W.; Jiang Y.; Li L. (2006)

  An appropriate form of induced polarization (IP) acts as a bridge between the structure of a water-saturated core plug and its transport properties. The induced-polarization decay curves of natural rocks can be modeled as ...
• THE MAGNETIC POLARITY TIME SCALE ACROSS THE PERMIAN-TRIASSIC BOUNDARY 

  Steiner M.B. (2006)

  Early Triassic and Late to Middle Permian magnetostratigraphic investigations are numerous and span the globe. More than 20 magnetostratigraphic sequences have documented all or part of the Early Triassic geomagnetic field ...

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