標(biāo)題: Titlebook: Basalts and Phase Diagrams; An Introduction to t Stearns A. Morse Textbook 2024Latest edition Springer Nature Switzerland AG 2024 Anorthite [打印本頁] 作者: FORAY 時間: 2025-3-21 17:13
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作者: 小步舞 時間: 2025-3-21 21:51 作者: 草本植物 時間: 2025-3-22 02:25
Stearns A. MorseDiscusses intensive parameters of mineral systems at high pressures.Covers fundamentals of physical chemistry applied to silicate liquids and crystals.Illustrates in detail the four limiting processes作者: CAPE 時間: 2025-3-22 06:52 作者: 無思維能力 時間: 2025-3-22 12:46 作者: 幻想 時間: 2025-3-22 16:55 作者: 出汗 時間: 2025-3-22 17:31
Weak Convergence and the Poisson Processat element is present. In this case, it is to be expected that diopside will steal Al from albite. The bad news does not end with this, for the albite will also steal Ca from diopside to make plagioclase, and the resulting effects on residual liquids are both important and difficult to analyse.作者: 樂意 時間: 2025-3-23 00:42
Crash Course I: Regular Variationava which pours out of Kilauea in Hawaii, and maybe crosses a tar road without melting it (we love to play that ace). Basalt is the rock that formed the island of Surtsey, off Iceland, as people watched. It springs up here and there on continents (Japan, USA in Washington or New York). The name is a作者: 使成整體 時間: 2025-3-23 01:47 作者: Encoding 時間: 2025-3-23 08:55 作者: Instinctive 時間: 2025-3-23 12:35
Weak Convergence and the Poisson Process phase rule. A working knowledge of the phase rule is essential for the effective use of phase diagrams. Such a working knowledge is very simple to acquire, since the phase rule is a very simple statement about the relationships of three variables. Like many rules, the phase rule conceals in its sim作者: Judicious 時間: 2025-3-23 14:33
Weak Convergence and the Poisson Processes a neat example of what may go wrong with a model when a mineral chooses not to have the idealized composition you so hopefully expected it would. This complication, fortunately, increases rather than decreases the relevance of the model system to natural basalts.作者: 表否定 時間: 2025-3-23 21:58
https://doi.org/10.1007/978-0-387-45024-7the Di-An model of basalts if we could study a model of Di-An., or in other words part of the ternary system Di-An-Ab. It would be folly to do this, however, without first examining the nature of all the binary combinations, An-Ab and Di-Ab as well as Di-An, already discussed.作者: 運動的我 時間: 2025-3-24 01:37
Weak Convergence and the Poisson Processat element is present. In this case, it is to be expected that diopside will steal Al from albite. The bad news does not end with this, for the albite will also steal Ca from diopside to make plagioclase, and the resulting effects on residual liquids are both important and difficult to analyse.作者: 歌劇等 時間: 2025-3-24 06:24 作者: 值得贊賞 時間: 2025-3-24 07:37
Inference and Empirical Examples,cium-poor pyroxene, but these are fundamentally important minerals in any classification scheme of basalt, and are furthermore centrally involved in our study model, the basalt tetrahedron (Chap. .). The present chapter explores a phase diagram containing iron-free olivine, namely forsterite, thereb作者: 聯(lián)想 時間: 2025-3-24 11:04 作者: abysmal 時間: 2025-3-24 14:54
https://doi.org/10.1007/978-90-481-9171-0y system. We shall now see that the incongruent melting of orthopyroxene in the system Fo-SiO. is carried over into a ternary system when a component such as anorthite is added. This ternary system is one of the most useful in illustrating the importance of the reaction relationship of olivine in ig作者: graphy 時間: 2025-3-24 19:01 作者: 有助于 時間: 2025-3-25 01:13 作者: 機制 時間: 2025-3-25 06:10
The tail empirical and quantile processesrelated to this system at 1?bar pressure. A brief discussion of the system nepheline–silica (NaAlSiO.-SiO.) serves to introduce the important principle of the thermal barrier (or thermal divide), which tends to prevent silica-undersaturated liquids from producing critically undersaturated residua an作者: Immunoglobulin 時間: 2025-3-25 10:40
Regularly varying random vectors small amounts of the orthoclase molecule, KAlSi.O.. Potassium is a large alkali ion (1.46?? radius if we use the compilation of radii by Whittaker and Muntus 1970), considerably larger than sodium (1.10??). Because of its large size, it is almost entirely excluded from the common mafic minerals of 作者: Sarcoma 時間: 2025-3-25 12:07 作者: orient 時間: 2025-3-25 19:50
,Die regelm??ige Schwangerschaft,temperatures appreciably, but in addition we find that fundamental changes occur in the reaction relation of olivine to pyroxene. The chapter opens with a review of the system MgO-FeO-SiO., taken in part from the original research paper. It then continues with an iron-bearing version of Fo-An-SiO., 作者: Flatus 時間: 2025-3-25 20:05 作者: 復(fù)習(xí) 時間: 2025-3-26 03:35 作者: debunk 時間: 2025-3-26 08:11 作者: 發(fā)電機 時間: 2025-3-26 11:23 作者: 使苦惱 時間: 2025-3-26 13:36
Diopside-Albite: A Complex System,at element is present. In this case, it is to be expected that diopside will steal Al from albite. The bad news does not end with this, for the albite will also steal Ca from diopside to make plagioclase, and the resulting effects on residual liquids are both important and difficult to analyse.作者: 青春期 時間: 2025-3-26 17:43 作者: 引起痛苦 時間: 2025-3-27 00:53
Incongruent Melting: The System Forsterite-Silica, + liquid equilibria En + Fo + . and En + Q + .. Instead, an important phenomenon exists near the plane, wherein the assemblage forsterite + . extends to more silica-rich compositions than the plane itself, with or without enstatite, thus providing a possibility for liquids to become silica-oversatu作者: jumble 時間: 2025-3-27 02:14 作者: 勤勞 時間: 2025-3-27 07:22 作者: circuit 時間: 2025-3-27 11:36 作者: 打谷工具 時間: 2025-3-27 15:50 作者: INCUR 時間: 2025-3-27 21:23 作者: 2否定 時間: 2025-3-27 23:54 作者: 導(dǎo)師 時間: 2025-3-28 03:36 作者: Cupping 時間: 2025-3-28 06:41
Prussia. Ministerium für Volkswohlfahrt publication is based on multiples of Pascals. Some Earthly journals still accept kbar for upper-crustal pressures. A summary of Earth pressures and mantle minerals versus depth is given in Table 18.1.作者: Arrhythmia 時間: 2025-3-28 11:10 作者: endocardium 時間: 2025-3-28 15:42 作者: ligature 時間: 2025-3-28 19:20
Forsterite-Anorthite-Silica: Incongruent Melting in a Ternary System,the role of the plane of silica saturation, modelled in this system by the line An-En. This role is like that of a check valve: liquids which pierce the plane towards SiO. cannot return, at atmospheric pressure, because of the incongruent melting of En to Fo + 作者: 外向者 時間: 2025-3-29 02:39
,Nepheline–Silica and the Rest of the Basalt Tetrahedron,ntal basalt tetrahedron. This review will serve as the background for examination, in succeeding chapters, of the effects of other components and of pressure on the phase relations of basaltic systems.作者: 侵略主義 時間: 2025-3-29 03:51
Textbook 2024Latest editionnd equilibrium crystallization are rigorously examined. Examples of the use of phase diagrams are drawn from the literature of layered intrusions, redox equilibria in iron-bearing systems, and the high pressure equilibria of melting in the mantle.作者: 失望未來 時間: 2025-3-29 11:11 作者: 被詛咒的人 時間: 2025-3-29 14:13 作者: FLACK 時間: 2025-3-29 15:36 作者: 無能的人 時間: 2025-3-29 19:53 作者: consolidate 時間: 2025-3-30 03:51
Inference and Empirical Examples,ur study model, the basalt tetrahedron (Chap. .). The present chapter explores a phase diagram containing iron-free olivine, namely forsterite, thereby illuminating some important principles of rock genesis as well as some simple but useful new principles of phase diagrams.作者: 愉快么 時間: 2025-3-30 04:07
Dealing with extremal independenceerved that will meet the upward layering rocks in what has been pleasantly named a sandwich horizon. Layered intrusions have important ways of revealing to us examples of phase equilibria that are fundamental. We only have to discover what these principles are.作者: 巨頭 時間: 2025-3-30 11:07 作者: 向外供接觸 時間: 2025-3-30 14:03
Prussia. Ministerium für Volkswohlfahrtdissolve only minute amounts of H.O. A system composed of an anhydrous phase plus H.O gas has a large volume just below the melting point, and the formation of hydrous melt will lead to a smaller volume above the melting point, so high pressure favours the formation of melt.作者: 不發(fā)音 時間: 2025-3-30 18:55
Introduction,he island of Surtsey, off Iceland, as people watched. It springs up here and there on continents (Japan, USA in Washington or New York). The name is applied to the solid rock, the lava, and to the magma which, on eruption, becomes lava.作者: 討厭 時間: 2025-3-31 00:45 作者: ARIA 時間: 2025-3-31 04:23
Crystals and Melts,or silicates (except quartz!), as we shall see below. The phenomena of melting and crystallization are unfamiliar to many readers, and the atomic organization and bonding of liquids turns out to have much importance for the theory and practice of melting.作者: MODE 時間: 2025-3-31 05:19 作者: 向外供接觸 時間: 2025-3-31 12:17
Layered Intrusions,erved that will meet the upward layering rocks in what has been pleasantly named a sandwich horizon. Layered intrusions have important ways of revealing to us examples of phase equilibria that are fundamental. We only have to discover what these principles are.作者: LIKEN 時間: 2025-3-31 13:34 作者: PANG 時間: 2025-3-31 18:53
Effects of Volatiles at High Pressure,dissolve only minute amounts of H.O. A system composed of an anhydrous phase plus H.O gas has a large volume just below the melting point, and the formation of hydrous melt will lead to a smaller volume above the melting point, so high pressure favours the formation of melt.作者: Thyroiditis 時間: 2025-4-1 01:32
esses of fractional and equilibrium melting and fractional and equilibrium crystallization are rigorously examined. Examples of the use of phase diagrams are drawn from the literature of layered intrusions, redox equilibria in iron-bearing systems, and the high pressure equilibria of melting in the mantle.978-3-030-97882-2作者: 感激小女 時間: 2025-4-1 05:11
Weak Convergence and the Poisson Processpter is to provide some fundamental definitions and a very rudimentary sketch of the principles upon which the phase rule rests. As we shall develop and use it, the phase rule is a part of what is called classical thermodynamic., the counterpart of which is statistical mechanics.作者: 窗簾等 時間: 2025-4-1 08:36
https://doi.org/10.1007/978-3-662-36582-3ntration of phosphorus becomes high enough to saturate the melt in apatite component. Present generally in minor quantities, phosphorus can be ignored for present purposes, always bearing in mind that its abundance level in basaltic magmas may contain important information, which we may or may not be able to analyse correctly.作者: agenda 時間: 2025-4-1 11:44
The Phase Rule as a Tool,pter is to provide some fundamental definitions and a very rudimentary sketch of the principles upon which the phase rule rests. As we shall develop and use it, the phase rule is a part of what is called classical thermodynamic., the counterpart of which is statistical mechanics.
