Titlebook: Argillaceous Rock Atlas; Neal R. O’Brien,Roger M. Slatt Book 1990 Springer-Verlag New York Inc. 1990 Sediment.Turbidite.diagenesis.fabric.

偏離

What it meant to be a Cimento academicianemical and microfabric conditions. Rickard indicates the spheroidal shape may be due to pseudomorphism of a pre-existing spherical body. It may represent replacement of an immiscible organic liquid globule by iron sulfide or infilling by microcrystalline pyrite of spherical gaseous vacuoles or even

POINT

What it meant to be a Cimento academicianaction (mechanical rearrangement of particles) in shale formation. It is commonly agreed that most clay-rich sediment settles out in sea water as aggregates or floccules. The “flocculated model” (see section on PREFERRED PARTICLE ORIENTATION IN SHALE) shows how parallel particles result from an orig

Prognosis

Giovanni Alfonso Borelli (1608–1679) or carbonate sediment that in its natural setting has generated and released enough hydrocarbons to form a commercial accumulation of oil or gas. Studies of source rocks have emphasized the organic fraction of the sediments and there is very little published information on the inorganic fraction. A

正式演說

Studies in History and Philosophy of Scienceressuring. Our investigation of geopressured shales is very preliminary so we hope that the examples presented here will stimulate additional research. The term “geopressure” is used to describe pore fluid pressures which are greater than hydrostatic pressure (the pressure equal to that of a column

傻瓜

輕快帶來危險

Infant

Asparagus

蠟燭

https://doi.org/10.1007/978-1-4612-3422-7Sediment; Turbidite; diagenesis; fabric; lacustrine; oil shale; petrography; petroleum geology; sedimentary

職業(yè)

Springer-Verlag New York Inc. 1990