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Titlebook: Evaporite Basins; Tadeusz M. Peryt Book 1987 Springer-Verlag Berlin Heidelberg 1987 Deformation.Sediment.Trias.diagenesis.environment.form

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11#
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0930-0317 Overview: 978-3-540-18679-3978-3-540-48069-3Series ISSN 0930-0317 Series E-ISSN 1613-2580
12#
發(fā)表于 2025-3-23 17:47:43 | 只看該作者
Facies models for Australian precambrian evaporites,ne basins have not been recognised in the Australian Precambrian. Not are there any records of potash salts,although the microcline often associated with Proterozoic evaporites may represent the resting place of the potassium from original potash minerals.
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Polymer-Based Amperometric Biosensors,olution from the salt lake to playa by gradual separating from seawater..Saline mineral zonation of both models appears as bulls-eye pattern zoning for an evaporite basin, and multicentral bulls-eye pattern for the whole platform.
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15#
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https://doi.org/10.1007/978-3-031-26731-4ne basins have not been recognised in the Australian Precambrian. Not are there any records of potash salts,although the microcline often associated with Proterozoic evaporites may represent the resting place of the potassium from original potash minerals.
16#
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17#
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https://doi.org/10.1007/978-1-4757-5070-6 scale and the evolution at a larger sequential scale depends upon which one of these factors becomes dominant. The general evolution results in a typical sedimentary cycle..The structural behavior of the Hercynian basement controls distribution and sometimes preservation of the depsits. Diagenesis
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