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Titlebook: Depositional Sedimentary Environments; With Reference to Te Hans-Erich Reineck,Indra Bir Singh Book 1980Latest edition Springer-Verlag Berl

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樓主: morphology
51#
發(fā)表于 2025-3-30 10:58:16 | 只看該作者
52#
發(fā)表于 2025-3-30 12:57:53 | 只看該作者
53#
發(fā)表于 2025-3-30 18:24:42 | 只看該作者
54#
發(fā)表于 2025-3-30 23:17:34 | 只看該作者
https://doi.org/10.1007/978-3-319-67876-4udation products. Associated with erosional environments are depositional environments, with their characteristic depositional processes and products of deposition (Walther 1894). In the geological record it is the depositional environment which leaves behind its imprints in sediment and produces se
55#
發(fā)表于 2025-3-31 02:39:32 | 只看該作者
Depositional Environmentsudation products. Associated with erosional environments are depositional environments, with their characteristic depositional processes and products of deposition (Walther 1894). In the geological record it is the depositional environment which leaves behind its imprints in sediment and produces se
56#
發(fā)表于 2025-3-31 05:06:51 | 只看該作者
Introductionlithosphere by volume, they occupy 75% of the exposed land area (Pettijohn 1957). Thus, the study of sedimentary rocks is the major problem of geology. An obvious question arises in the study of sedimentary rocks: Under what conditions and by which processes were the sedimentary rocks in question de
57#
發(fā)表于 2025-3-31 10:16:14 | 只看該作者
Depositional Environments study the environment of igneous rocks i.e., the physico-chemical environment of their formation, or the environment of metamorphic rocks and minerals which deals with the study of stability of various minerals under different pressure-temperature conditions, or the environment of sedimentary rocks
58#
發(fā)表于 2025-3-31 15:30:59 | 只看該作者
59#
發(fā)表于 2025-3-31 20:11:01 | 只看該作者
Current and Wave Ripplesduced as a result of the interaction of waves or currents on a sediment surface. Ripple marks are one of the commonest features of sedimentary rocks, both in Recent and ancient sediments. The shape and size of ripples vary considerably. The crests usually run parallel to each other or may anastomose
60#
發(fā)表于 2025-4-1 01:05:19 | 只看該作者
Surface Markings and Imprints with a well-formed central crater made up of sand and silt ejected from the central vent. They form by springs welling up through quicksand, quickmud (Fig. 68), or slumped material (Gill and Kuenen 1958). Sediment volcanoes are associated with the expulsion of water from sediment as a result of slu
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