標(biāo)題: Titlebook: Chemical Transport in Metasomatic Processes; Harold C. Helgeson Book 1987 Springer Science+Business Media Dordrecht 1987 Mafic.chemistry.e [打印本頁] 作者: Kennedy 時(shí)間: 2025-3-21 17:34
書目名稱Chemical Transport in Metasomatic Processes影響因子(影響力)
書目名稱Chemical Transport in Metasomatic Processes影響因子(影響力)學(xué)科排名
書目名稱Chemical Transport in Metasomatic Processes網(wǎng)絡(luò)公開度
書目名稱Chemical Transport in Metasomatic Processes網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Chemical Transport in Metasomatic Processes被引頻次
書目名稱Chemical Transport in Metasomatic Processes被引頻次學(xué)科排名
書目名稱Chemical Transport in Metasomatic Processes年度引用
書目名稱Chemical Transport in Metasomatic Processes年度引用學(xué)科排名
書目名稱Chemical Transport in Metasomatic Processes讀者反饋
書目名稱Chemical Transport in Metasomatic Processes讀者反饋學(xué)科排名
作者: 浪費(fèi)時(shí)間 時(shí)間: 2025-3-21 23:22 作者: Figate 時(shí)間: 2025-3-22 00:23 作者: Consequence 時(shí)間: 2025-3-22 07:18
Fluid Inclusions and Pressure-Temperature Estimates in Deep-Seated Rocksions studies to a state approaching maturity. The number of well studied cases remains, however, limited, and many researchers hesitate to engage in a type of study that they consider highly specialized, time consuming and with questionable results. The different steps of fluid inclusion studies of 作者: 易達(dá)到 時(shí)間: 2025-3-22 11:46 作者: 謊言 時(shí)間: 2025-3-22 13:33
Metasomatism Involving Fluids in CO2-H2O-NaClng most temperature-depth paths in metamorphic rocks if the chloride content of the fluid system is adequate. The presence of, two fluid phases is shown to have considerable influence on the evolution of fluid composition in reacting metasomatic systems. An aqueous brine interacting with dehydration作者: 謊言 時(shí)間: 2025-3-22 17:21 作者: Harbor 時(shí)間: 2025-3-22 21:55
A Simple Thermodynamic Model for Grain Interfaces: Some Insights on Nucleation, Rock Textures, and Mwithin the validity of the model, characterize an equilibrium texture. These include “Wulff’s Law” for the equilibrium form of a crystal in a fluid, and also a rule of indentation that has features in common with Becke’s concept of a “crystalloblastic series.” The model also leads to simple expressi作者: Cosmopolitan 時(shí)間: 2025-3-23 04:58
Application of Moderation Theorems to Metasomatic Processes. Although in the absence of external constraints, the moderation theorem known as the Le Chatelier-Braun principle affords accurate prediction of the consequences of such perturbations in closed systems, it is not applicable to many reactions of geologic interest in open systems. As demonstrated by作者: HEDGE 時(shí)間: 2025-3-23 08:10 作者: Irremediable 時(shí)間: 2025-3-23 09:52 作者: Laconic 時(shí)間: 2025-3-23 13:57 作者: chondromalacia 時(shí)間: 2025-3-23 18:38
Controls of the Chemical Composition of Geothermal Watersr with secondary minerals resulting from water-rock interaction. Simple calculations of the composition of water at equilibrium can be performed by using the concept of complete mineral association : the number of minerals is equal to the number of major inert elements in the solution. For each elem作者: GROSS 時(shí)間: 2025-3-23 23:46 作者: ALT 時(shí)間: 2025-3-24 06:03 作者: tendinitis 時(shí)間: 2025-3-24 10:25 作者: Obloquy 時(shí)間: 2025-3-24 13:04
Lagrangian and Eulerian Representations of Metasomatic Alteration of Minerals on a continuum representation of porous media. The Eulerian method is an inherently transient description of advective and diffusive/dispersive transport referred to a reference frame that is fixed with respect to the rock mass. The Lagrangian method, applicable to flowing systems, is referred to a作者: cortisol 時(shí)間: 2025-3-24 16:40 作者: 妨礙 時(shí)間: 2025-3-24 20:21 作者: 輕推 時(shí)間: 2025-3-24 23:19
978-94-010-8280-8Springer Science+Business Media Dordrecht 1987作者: Canyon 時(shí)間: 2025-3-25 06:30 作者: 最高點(diǎn) 時(shí)間: 2025-3-25 11:17 作者: modifier 時(shí)間: 2025-3-25 12:26 作者: adroit 時(shí)間: 2025-3-25 17:11 作者: 形容詞詞尾 時(shí)間: 2025-3-25 21:16 作者: 使混合 時(shí)間: 2025-3-26 03:51
Progress in Location-Based Services 2016basalts and kimberlites are interpreted as non-equilibrium phenomena. The mantle nodules exhibit data arrays that cut steeply across the Δ.O = zero line on such δ-δ diagrams. These arrays resemble the non-equilibrium quartz-feldspar and feldspar-pyroxene δ.O arrays that we now know are . of hydrothe作者: 無禮回復(fù) 時(shí)間: 2025-3-26 05:27 作者: indifferent 時(shí)間: 2025-3-26 09:53 作者: 侵略者 時(shí)間: 2025-3-26 14:29
Progress in Marine Conservation in Europeions studies to a state approaching maturity. The number of well studied cases remains, however, limited, and many researchers hesitate to engage in a type of study that they consider highly specialized, time consuming and with questionable results. The different steps of fluid inclusion studies of 作者: orthodox 時(shí)間: 2025-3-26 17:24
H. J. Dudek,W. Braue,G. Zieglers the role of fluid as it carries chemical components from one environment into another; metasomatism refers to changes in rock composition. This communication discusses the relationship between fluid transport and the local reactions among minerals and the aqueous phase. At even modest flow rates, 作者: 的是兄弟 時(shí)間: 2025-3-26 21:22
K. H. Koch,D. Sommer,D. Grunenbergng most temperature-depth paths in metamorphic rocks if the chloride content of the fluid system is adequate. The presence of, two fluid phases is shown to have considerable influence on the evolution of fluid composition in reacting metasomatic systems. An aqueous brine interacting with dehydration作者: 男學(xué)院 時(shí)間: 2025-3-27 02:14
K. H. Koch,D. Sommer,D. Grunenbergfferent stages of pro-grade metamorphism. At constant pressure, a rock that generates a larger volume of fluid than its neighbour will tend to export fluid to its neighbour, particularly if the boundary between the two is not absolutely impermeable. The invasion of one rock by the fluid from another作者: 取消 時(shí)間: 2025-3-27 05:53 作者: 全面 時(shí)間: 2025-3-27 13:24 作者: 都相信我的話 時(shí)間: 2025-3-27 16:06 作者: 開始發(fā)作 時(shí)間: 2025-3-27 21:03
Measurement of Human Body Composition ,, two continents are discussed and compared in order to answer the question put in the title: 1. Corundum-fuchsite rocks from Archaean greenstone belts in Southern Africa with Al.O.- contents up to 85 % and high Cr.O. occurring within ultramafic bodies as transgressive masses are found to be metamorp作者: 舔食 時(shí)間: 2025-3-28 01:30
Ettore Majorana International Science Serieshe system K.O-Al.O.-SiO. (figure 1) such as quartz-feldspar-muscovite, muscovite-leucite-corundum, and several others. We interpret the results as indicating that the solutes are dominantly uncharged species, specifically alkali-alumina and alkalialumina- silica species.作者: infantile 時(shí)間: 2025-3-28 03:53
https://doi.org/10.1007/978-1-4899-0809-4r with secondary minerals resulting from water-rock interaction. Simple calculations of the composition of water at equilibrium can be performed by using the concept of complete mineral association : the number of minerals is equal to the number of major inert elements in the solution. For each elem作者: 上下連貫 時(shí)間: 2025-3-28 09:29 作者: 文藝 時(shí)間: 2025-3-28 11:20 作者: 大包裹 時(shí)間: 2025-3-28 18:35
High Myopia Requires “High Attention” on fluid composition and fluid behaviour during the M2-metamorphism (mainly Naxos), and the M3-metamorphism (Serifos). Fluids during the M2 metamorphism on Naxos are mixed CO.-H.O fluids, with remarkably constant chemical and carbon isotopic composition, over the whole range of temperatures and lit作者: 獨(dú)行者 時(shí)間: 2025-3-28 22:19
Progress in Myopia Prevention and Control on a continuum representation of porous media. The Eulerian method is an inherently transient description of advective and diffusive/dispersive transport referred to a reference frame that is fixed with respect to the rock mass. The Lagrangian method, applicable to flowing systems, is referred to a作者: Graphite 時(shí)間: 2025-3-28 23:11 作者: BROOK 時(shí)間: 2025-3-29 03:46 作者: Trypsin 時(shí)間: 2025-3-29 08:26 作者: hemorrhage 時(shí)間: 2025-3-29 15:14
18O/16O Evidence for Fluid-Rock Interaction in the Upper Mantle: Data from Ultramafic Nodules and K-with the equilibrium interpretation. The metasomatic .O-enrichments of the peridotites can be related to metasomatic enrichments in LIL elements and the development of amphibole and phlogopite. In recent studies of leucite-bearing lavas with .Sr/.Sr = 0.7102 to 0.7106 from the Alban Hills and M. Vul作者: 不安 時(shí)間: 2025-3-29 16:42 作者: 厚顏無恥 時(shí)間: 2025-3-29 21:20
Metasomatism of the Continental Lithosphere: Simulation of Isotope and Element Abundance Behaviour atope systematics can be accounted for. Identification of fluid and solid end-members suggest for both volcanic provinces that fluids which presumably had their origin in the asthenosphere invaded, penetrated and metasomatised the lithospheric mantle and crustal material, which may be previously subd作者: 認(rèn)為 時(shí)間: 2025-3-30 01:36 作者: fetter 時(shí)間: 2025-3-30 04:14 作者: 緊張過度 時(shí)間: 2025-3-30 11:07
Application of Moderation Theorems to Metasomatic Processesocesses. Although moderation with respect to the mole fraction of a perturbed component always occurs in fluids in which ideal mixing takes place, whether or not moderation of metasomatic reactions takes place with respect to addition to, or removal from the fluid of a small amount of a given compon作者: 假裝是你 時(shí)間: 2025-3-30 14:49
Induced Stress and Secondary Mass Transfer: Thermodynamic Basis for the Tendency toward Constant-Volential gradients are induced by the stress field. To the extent that “secondary” mass transfer is driven by such gradients, the induced stress-field tends to relax towards constant and uniform pressure. If the secondary mass transfer is so efficient that the induced stress never rises to the thresho作者: Nmda-Receptor 時(shí)間: 2025-3-30 19:31
Pre- or Synmetamorphic Metasomatism in Peraluminous Metamorphic Rocks?O. up to 77 %, and associated topazites, tourmaline, and dumortierite rocks may be best explained by near-surface, postvolcanic rock alteration of a thick, slowly cooling ignimbrite unit, combined with subsequent deposition of Al-rich products in an evaporitic environment. However, there is also tex作者: 秘傳 時(shí)間: 2025-3-30 22:56 作者: 致詞 時(shí)間: 2025-3-31 03:35 作者: troponins 時(shí)間: 2025-3-31 08:19 作者: 等待 時(shí)間: 2025-3-31 11:13
Metamorphic Events in the Cyclades and their Associated Fluidsn at Serifos (M3) are extremely saline brines containing NaCl-CaCl.-MgCl.-KCl-FeCl.. Geological and isotopic evidence is in favour of a magmatic origin of these fluids, which have caused extensive skarn formation in and around the granodiorite.作者: vibrant 時(shí)間: 2025-3-31 15:34
Lagrangian and Eulerian Representations of Metasomatic Alteration of Mineralsn and diffusion based on the Eulerian formulation, are compared with results obtained from a single Lagrangian fluid packet. Following a transient period during which mineral reaction products pyrophyllite and kaolinite precipitate and redissolve, the Eulerian calculation results in the formation of作者: Alopecia-Areata 時(shí)間: 2025-3-31 21:13 作者: Chagrin 時(shí)間: 2025-3-31 23:20
Progress in Location-Based Services 2016with the equilibrium interpretation. The metasomatic .O-enrichments of the peridotites can be related to metasomatic enrichments in LIL elements and the development of amphibole and phlogopite. In recent studies of leucite-bearing lavas with .Sr/.Sr = 0.7102 to 0.7106 from the Alban Hills and M. Vul
