Titlebook: Carbonate Microfabrics; Richard Rezak (Professor Emeritus),Dawn L. Lavoie Book 1993 Springer-Verlag New York, Inc. 1993 chemistry.fabric.g

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Preferred Orientation and Velocity Anisotropy in Marine Clay-Bearing Calcareous Sedimentss, ultrasonic .. and x-ray pole figure goniometry measurements were made on selected laminated calcareous claystones, laminated clay-bearing limestones, and nonlaminated limestones from various DSDP sites. Although all samples exhibit .. anisotropy (up to 20%), none exhibit calcite-preferred orienta

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Stress-Deformation Behavior of Two Carbonate Oozesained from the vicinity of the Christmas and Fanning Islands in the Pacific. Both sediments consisted of fine sand- to silt-sized carbonate foraminiferal and nannofossil oozes with 88 to 93% calcium carbonate. The samples had high water contents (89 to 127%), exhibited some plasticity, and were very

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Microfabric and Compositional Clues to Dominant Mud Mineralogy of Micrite Precursorsbric and composition in micrites may be related to the original mineralogy of the precursor lime mud. This chapter takes a broader look at Cenozoic (mainly Plio-Pleistocene) micritic limestones to evaluate the role of original mineralogy in the evolution of microfabric and composition in fine-graine

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Recrystallization of Dolomite with Timeicantly from those modern dolomites proposed as analogs for their genesis. Application of modern analogs to the origin of ancient dolomites all too often presumes that present-day fabrics and chemistries record conditions prevailing at the time of precipitation. Petrographic (plane-light and cathodo

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https://doi.org/10.1007/978-1-4684-9421-1chemistry; fabric; geochemistry; geology; geophysics

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Springer-Verlag New York, Inc. 1993

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https://doi.org/10.1007/978-1-4612-1432-8g both light and electrons, can be said to define the modern era of microfabric studies. Since 1950 the attention of research workers has veered from one topic to another, qualifying old dogmas and embracing new ones, in a continual struggle to explain what the microscope reveals. The philosopher A.

商谈

Three-Term Conjugate Gradient Methods,le, dune and beach sands display pronounced development of subaerial microfabric features. Pleistocene grainstones from San Salvador, Bahamas, contain rhizoliths, pedotubules, alveolar textures, calcified root hairs, Microcodium, laminated micrite, clotted micrite, soil pisoids, circumgranular crack