Titlebook: Clays in Crustal Environments; Isotope Dating and T Norbert Clauer,Sambhu Chaudhuri Book 1995 Springer-Verlag Berlin Heidelberg 1995 Clay M

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整潔漂亮

panorama

Isotope Geochemistry of Clay Minerals in Young Continental and Oceanic Sediments, are deposited in fluvial, glacial, lacustrine and other continental depositional centers and in various parts of the oceanic basins, the latter constituing almost the bulk of the sediments deposited during the entire history of the Earth. A recent estimate given by Milliman and Meade (1983) suggest

Tonometry

Isotope Geochemistry of Clays and Clay Minerals from Sedimentary Rocks,s either syn-depositional or post-depositional, but the distinction between them in an ancient sedimentary rock is not always easy. This distinction is important because only the isotopic records of very early authigenic minerals may be examined to determine the time of deposition of the sediments.

不能平靜

Isotope Geochemistry of Mica-Type Minerals from Low-Temperature Metamorphic Rocks,ch very often consist in mixed suites of detrital and authigenic minerals. The chaotic isotopic relationship that is very common among different components in sedimentary rocks begins to give way to a relatively more coherent relationship among evolved components with the onset of metamorphism. Many

熱心

The Frontiers of Clay Isotope Geochemistry, also represent the most fascinating component of this complex “chemical world”, because they carry records of many discrete evolutionary events in the constantly changing history of the upper crust. Isotopic data gathered from analyses of clay minerals can, therefore, serve as very useful tracers f

熱心

ntary deposits, and under regional, contact and hydrothermal metamorphism conditions..The book provides information about the dynamics of isotope systems in clays and helps us to understand the physical and chemical parameters in the transfer of masses within the crustal domain. Written for graduate

ARCH

騎師

Isotope Geochemistry of Mica-Type Minerals from Low-Temperature Metamorphic Rocks,nents in sedimentary rocks begins to give way to a relatively more coherent relationship among evolved components with the onset of metamorphism. Many metasedimentary rocks afford excellent opportunities to study the characters of dynamism of different isotopes in clays subjected to a wide variety of low-temperature metamorphic environments.

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