標題: Titlebook: Clays in Crustal Environments; Isotope Dating and T Norbert Clauer,Sambhu Chaudhuri Book 1995 Springer-Verlag Berlin Heidelberg 1995 Clay M [打印本頁] 作者: 味覺沒有 時間: 2025-3-21 18:41
書目名稱Clays in Crustal Environments影響因子(影響力)
書目名稱Clays in Crustal Environments影響因子(影響力)學科排名
書目名稱Clays in Crustal Environments網(wǎng)絡(luò)公開度
書目名稱Clays in Crustal Environments網(wǎng)絡(luò)公開度學科排名
書目名稱Clays in Crustal Environments被引頻次
書目名稱Clays in Crustal Environments被引頻次學科排名
書目名稱Clays in Crustal Environments年度引用
書目名稱Clays in Crustal Environments年度引用學科排名
書目名稱Clays in Crustal Environments讀者反饋
書目名稱Clays in Crustal Environments讀者反饋學科排名
作者: 整潔漂亮 時間: 2025-3-21 22:37 作者: panorama 時間: 2025-3-22 04:05
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作者: Tonometry 時間: 2025-3-22 08:01
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. 作者: 不能平靜 時間: 2025-3-22 10:46
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作者: 熱心 時間: 2025-3-22 13:38
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作者: 熱心 時間: 2025-3-22 20:05
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作者: ARCH 時間: 2025-3-22 23:12 作者: 騎師 時間: 2025-3-23 03:39
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.作者: commonsense 時間: 2025-3-23 05:59 作者: Common-Migraine 時間: 2025-3-23 10:46
students taking courses in sedimentary geochemistry, clay mineralogy, and soil mineralogy, the book will also appeal to scientists carrying out research on clay genesis and mass transfer in crustal environments.978-3-642-79087-4978-3-642-79085-0作者: tolerance 時間: 2025-3-23 14:15
Book 1995sits, 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 students 作者: octogenarian 時間: 2025-3-23 18:06
Resilience: A New Paradigm of Nuclear Safetysediment into sedimentary rocks. Weathering is the beginning of the exogenic cycle, initiated by chemical alteration and physical breakdown of rocks and minerals at or near the surface of the Earth. The process of alteration and breakdown is then followed by various processes of denudation.作者: 蓋他為秘密 時間: 2025-3-23 23:02
https://doi.org/10.1007/978-3-319-58768-4nsist of <2 μm size particles. Assuming that nearly 60% of the <2 μm fraction consists of clay minerals, which is the same amount present in an average shale, about 2.4 × 10.kg of clay minerals are delivered each year to the present-day oceans by the rivers.作者: CON 時間: 2025-3-24 02:43
Isotope Geochemistry of Clay Minerals in Continental Weathering Environments,sediment into sedimentary rocks. Weathering is the beginning of the exogenic cycle, initiated by chemical alteration and physical breakdown of rocks and minerals at or near the surface of the Earth. The process of alteration and breakdown is then followed by various processes of denudation.作者: micronized 時間: 2025-3-24 07:09 作者: Foam-Cells 時間: 2025-3-24 14:32
Isotope Geochemistry of Clays and Clay Minerals from Sedimentary Rocks,nerals in question that might have been subjected to varied depositional and post-depositional forces causing modifications in physical and chemical aspects of a mass of sediment (Clauer et al. 1992c).作者: Hiatus 時間: 2025-3-24 17:45
The Frontiers of Clay Isotope Geochemistry,ot be taken as straightforward information about the history of their formation. Because the growth of clay minerals often results from replacement of silicate precursors, the reaction rate is an important control in determining the isotopic signatures of the newly formed clay phases.作者: 反應(yīng) 時間: 2025-3-24 22:59
Resilience: A New Paradigm of Nuclear Safetynerals in question that might have been subjected to varied depositional and post-depositional forces causing modifications in physical and chemical aspects of a mass of sediment (Clauer et al. 1992c).作者: Obstruction 時間: 2025-3-25 00:19 作者: Glossy 時間: 2025-3-25 03:40 作者: addict 時間: 2025-3-25 10:41 作者: 裁決 時間: 2025-3-25 11:58 作者: 柱廊 時間: 2025-3-25 19:22 作者: 胰臟 時間: 2025-3-25 21:16 作者: 吹牛大王 時間: 2025-3-26 04:03
Eliminiating Recurring Voltage Emergencies, 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作者: Amplify 時間: 2025-3-26 05:15
https://doi.org/10.1007/978-3-642-79085-0Clay Minerals; Crustal Environements; Diagenese; Diagenesis; Isotope; Isotopengeologie; Metamorphic Condit作者: exclusice 時間: 2025-3-26 11:02
978-3-642-79087-4Springer-Verlag Berlin Heidelberg 1995作者: hemorrhage 時間: 2025-3-26 13:49 作者: 正論 時間: 2025-3-26 20:19
http://image.papertrans.cn/c/image/227271.jpg作者: LATER 時間: 2025-3-26 20:59 作者: Chandelier 時間: 2025-3-27 04:55
9樓作者: 變量 時間: 2025-3-27 06:20
9樓作者: diskitis 時間: 2025-3-27 12:39
10樓作者: 到婚嫁年齡 時間: 2025-3-27 15:55
10樓作者: 防止 時間: 2025-3-27 18:15
10樓作者: ALIEN 時間: 2025-3-27 22:56
10樓
