作者: lactic 時間: 2025-3-21 20:53 作者: Gerontology 時間: 2025-3-22 04:20 作者: calumniate 時間: 2025-3-22 04:50 作者: uveitis 時間: 2025-3-22 08:46 作者: 貪心 時間: 2025-3-22 16:07
Book 1980Latest editionhis book is still unsurpassed in providing a good, basic synthesis of modern sedimentary environments, especially the physical attributes of the deposits being formed and the processes responsible..." (Sedimentary Geology).作者: 貪心 時間: 2025-3-22 19:51 作者: 太空 時間: 2025-3-22 22:15
Book 1980Latest editiond text, and gives excellent factual information on a large number of topics.".(Palaeogeography, Palaeoclimatology, Palaeoecology)."...represents a significant contribution to the literature of geoscience. It should be in the library of anyone seriously intereted in sedimentology."(Marine Geology)."T作者: Diaphragm 時間: 2025-3-23 01:40
Sediment Grain Parametersolled by the hydrodynamic conditions existing at the time of deposition. There have been repeated attempts to use such grain parameters as environmental indicators. In the following, a short account of various attempts in this direction and their limitations are given.作者: Genome 時間: 2025-3-23 06:27
Glacial Environmentof glacial deposits. This knowledge can be successfully applied in the study of ancient, e.g., pre-Pleistocene glacial deposits. Today, the glacial environment is restricted to areas around the north and south poles, and high mountains in other latitudes covered by snow e. g., the Alps and the Himalayas.作者: Presbyopia 時間: 2025-3-23 10:34
Desert Environmenth conditions, like position of the area within wind systems of natural low humidity, the presence of a mountain chain in the path of rain-bringing winds, the absence of sufficient relief to induce rainfall, etc.作者: 殘暴 時間: 2025-3-23 15:03 作者: 語源學 時間: 2025-3-23 18:03
Hardware Implementation of HS1-SIVn expulsion of water. Sediment in these rising columns of water becomes mobile, acting as quicksand or quickmud, and moves up to the sediment surface in form of a cone. The sediment columns formed on top of the compaction zone and the adjoinig cones or vents on the sediment surface may be preserved.作者: accessory 時間: 2025-3-23 23:22 作者: 預防注射 時間: 2025-3-24 03:18
Depositional Sedimentary Environments978-3-642-81498-3Series ISSN 0172-6234 作者: 使腐爛 時間: 2025-3-24 08:44
E-Business and Telecommunicationslithosphere 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 deposited.作者: ANNUL 時間: 2025-3-24 14:44
Jordi Cucurull,Sandra Guasch,David Galindond textures of a sediment are the major features that provide information about the medium and mode of transport (by ice, water, or wind) and energy conditions at the time of deposition. Energy conditions include depth of water, velocity of flow, turbulence, wind velocity, etc. The study of physical parameters can be divided into two groups.作者: 畸形 時間: 2025-3-24 15:17 作者: 侵略 時間: 2025-3-24 21:09 作者: Intend 時間: 2025-3-25 01:21 作者: travail 時間: 2025-3-25 05:39 作者: output 時間: 2025-3-25 08:11 作者: AVOID 時間: 2025-3-25 15:17
Sandra Díaz-Santiago,Debrup ChakrabortyBedding is perhaps the most important feature of a sedimentary rock, and is thus the most widely used term in describing a sedimentary sequence. Despite the importance of bedding in sedimentary rocks, no completely satisfactory or agreed-upon classification of bedding yet exists.作者: perjury 時間: 2025-3-25 19:14
Host Identity Detection in IPv6 NetworksEach modern environment or subenvironment is usually characterized by a given fauna, i. e., a biocoenosis inhabiting the region. Palaeontologists refer to such regions as biofacies. Upon death, burial, and preservation, a biocoenose (cf. Sch?fer 1963; Frey 1971; Sarjeant 1975) leaves behind:作者: 揮舞 時間: 2025-3-25 22:45 作者: 發(fā)出眩目光芒 時間: 2025-3-26 04:06 作者: BRAWL 時間: 2025-3-26 06:49
BeddingBedding is perhaps the most important feature of a sedimentary rock, and is thus the most widely used term in describing a sedimentary sequence. Despite the importance of bedding in sedimentary rocks, no completely satisfactory or agreed-upon classification of bedding yet exists.作者: output 時間: 2025-3-26 10:15 作者: 傲慢物 時間: 2025-3-26 14:53 作者: 向外才掩飾 時間: 2025-3-26 20:24 作者: urethritis 時間: 2025-3-26 23:38
https://doi.org/10.1007/978-3-642-81498-3Coast; Deformation; Ocean; Sediment; ecology; fluvial; geoscience; marine; marine geology作者: 館長 時間: 2025-3-27 04:14
978-3-540-10189-5Springer-Verlag Berlin Heidelberg 1980作者: 不可知論 時間: 2025-3-27 06:12
E-Business and Telecommunicationslithosphere 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作者: 匍匐 時間: 2025-3-27 09:49 作者: Delectable 時間: 2025-3-27 15:17 作者: 不能逃避 時間: 2025-3-27 17:46
E-Business and Telecommunicationsduced 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作者: 星星 時間: 2025-3-27 22:59
Hardware Implementation of HS1-SIV 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作者: 賞錢 時間: 2025-3-28 02:07 作者: 語源學 時間: 2025-3-28 08:12 作者: 全能 時間: 2025-3-28 13:42 作者: commodity 時間: 2025-3-28 17:19
Lassi Korhonen,Keijo Ruotsalainenare controlled partly by the environment of deposition. In the same way, the maximum grain size, grain-size distribution, fabric, etc., are also controlled by the hydrodynamic conditions existing at the time of deposition. There have been repeated attempts to use such grain parameters as environment作者: 革新 時間: 2025-3-28 22:18 作者: 說不出 時間: 2025-3-28 23:04
Anne Bouillard,Claude Jard,Aurore Junierlizations regarding distribution of bedding types are made. However, the critical reader is referred to Part I, where their distribution and genesis have been described. The utility of such models would be proved by critical study of such models in the light of study of ancient environments.作者: 領巾 時間: 2025-3-29 03:13 作者: LARK 時間: 2025-3-29 11:13 作者: itinerary 時間: 2025-3-29 13:22 作者: labile 時間: 2025-3-29 19:26
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 deposited.作者: 巧思 時間: 2025-3-29 22:28
Physical Parametersnd textures of a sediment are the major features that provide information about the medium and mode of transport (by ice, water, or wind) and energy conditions at the time of deposition. Energy conditions include depth of water, velocity of flow, turbulence, wind velocity, etc. The study of physical parameters can be divided into two groups.作者: Petechiae 時間: 2025-3-30 01:19 作者: 公社 時間: 2025-3-30 06:28 作者: 冰雹 時間: 2025-3-30 10:58 作者: 泄露 時間: 2025-3-30 12:57 作者: MILK 時間: 2025-3-30 18:24 作者: 莎草 時間: 2025-3-30 23:17
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作者: 符合國情 時間: 2025-3-31 02:39
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作者: larder 時間: 2025-3-31 05:06
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作者: 圍裙 時間: 2025-3-31 10:16
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作者: unstable-angina 時間: 2025-3-31 15:30 作者: heirloom 時間: 2025-3-31 20:11
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作者: 有偏見 時間: 2025-4-1 01:05
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作者: 胡言亂語 時間: 2025-4-1 04:04
