標題: Titlebook: Equilibrium and Kinetics in Contact Metamorphism; The Ballachulish Ign Gerhard Voll,Jutta T?pel,Friedrich Seifert Book 1991 Springer-Verlag [打印本頁] 作者: Grant 時間: 2025-3-21 18:13
書目名稱Equilibrium and Kinetics in Contact Metamorphism影響因子(影響力)
書目名稱Equilibrium and Kinetics in Contact Metamorphism影響因子(影響力)學(xué)科排名
書目名稱Equilibrium and Kinetics in Contact Metamorphism網(wǎng)絡(luò)公開度
書目名稱Equilibrium and Kinetics in Contact Metamorphism網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Equilibrium and Kinetics in Contact Metamorphism被引頻次
書目名稱Equilibrium and Kinetics in Contact Metamorphism被引頻次學(xué)科排名
書目名稱Equilibrium and Kinetics in Contact Metamorphism年度引用
書目名稱Equilibrium and Kinetics in Contact Metamorphism年度引用學(xué)科排名
書目名稱Equilibrium and Kinetics in Contact Metamorphism讀者反饋
書目名稱Equilibrium and Kinetics in Contact Metamorphism讀者反饋學(xué)科排名
作者: GLIB 時間: 2025-3-21 21:06
Structure, Petrography and Emplacement of Plutonic Rocksding a core of porphyritic granite with hybrid margins. Mesotype members of this suite are constituted of alkaline hypersthene diorites. This provides an unique opportunity to quantify the magmatic crystallization sequence within a relatively “dry” plutonic environment at upper crustal level, in ter作者: 浸軟 時間: 2025-3-22 02:52 作者: glans-penis 時間: 2025-3-22 07:57
Nucleation and Growth of Pyroxene in the Hypersthene Dioritese hypersthene-bearing monzodiorites are nearest to the contact. These relatively ‘dry’ diorites are least affected by late- to post-magmatic hydration southeast of Sgorr Dhonuill, where a very fine-grained chilled marginal facies bordered quartzitic country rocks, before the emplacement of granitic 作者: Opponent 時間: 2025-3-22 10:58 作者: HUSH 時間: 2025-3-22 15:50 作者: HUSH 時間: 2025-3-22 18:31 作者: 祖?zhèn)?nbsp; 時間: 2025-3-22 22:40 作者: DEAF 時間: 2025-3-23 04:02 作者: 膝蓋 時間: 2025-3-23 08:46
Petrography and Mineral Chemistry of Pelitescally within the zone of partial melting (Harte et al., Chap. 9, this Vol.) and within pelitic screens within the igneous complex. The two grids, when linked, provide a continuous petrogenetic grid from the lowest to highest grade in the aureole. In Pattison (Chap. 16, this Vol.) the continuous grid is calibrated in P-T space.作者: hidebound 時間: 2025-3-23 10:47
Book 1991ologists are no longer satisfied knowing the pressure-tempera- ture conditions of the formation of a metamorphic rock or of the emplace- ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it t作者: Euphonious 時間: 2025-3-23 16:20
focus: geologists are no longer satisfied knowing the pressure-tempera- ture conditions of the formation of a metamorphic rock or of the emplace- ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and r作者: 態(tài)學(xué) 時間: 2025-3-23 20:20 作者: 擋泥板 時間: 2025-3-24 01:51
Alfredo Pasquarello,Antonio Quattropanice of talc + calcite in siliceous dolomites and impure limestones. In the inner aureole from the point where both forsterite and diopside are formed, the outcrop is continuous up to the formation of periclase.作者: 別炫耀 時間: 2025-3-24 03:04
Thermal Conditions and Crystallization Sequence, as Deduced from Whole-Rock and Mineral Chemistryistry, phase relationships and geothermometry (Sect. 4.2; see Weiss and Troll 1989 for further details). The implications for fluid activity and the order of crystallization (Sect. 4.3, Fig. 4.11) are given ahead of a comprehensive summary on the petrogenesis of the Ballachulish pluton (Sect. 4.4).作者: Multiple 時間: 2025-3-24 09:11
Decarbonation Reactions in Siliceous Dolomites and Impure Limestonesce of talc + calcite in siliceous dolomites and impure limestones. In the inner aureole from the point where both forsterite and diopside are formed, the outcrop is continuous up to the formation of periclase.作者: 粗糙 時間: 2025-3-24 13:41 作者: Tracheotomy 時間: 2025-3-24 18:17 作者: uncertain 時間: 2025-3-24 19:25
Advanced 2D Rasterization on Modern CPUs,3.2 deals with contact relationships, xenoliths and foliation structures, followed by a modal classification of the igneous units (Sect. 3.3.1). A detailed petrography of index minerals, their texture and areal distribution (Sect. 3.3.2) precede the synoptical Sect. 3.4 on magma emplacement and intrusion mechanics.作者: overbearing 時間: 2025-3-25 02:09
https://doi.org/10.1007/978-3-319-64453-0rained rock, enclosing and grading into the relatively coarser inner parts of an intrusion” (Cox et al. 1979). Figure 5.1 attempts a reconstruction of the monzodiorite main zone before the emplacement of younger granites, omitting the large ring-dyke granite apophysis and correcting for later sinistral fault displacement (compare Fig. 3.13c).作者: 外表讀作 時間: 2025-3-25 06:55
https://doi.org/10.1007/978-3-642-18979-1tion, and their implications for the rheological and crystallization behaviour of the melts. The reader is referred to Pattison and Harte (1985, 1988; Sect. 8.5, this Vol.) for notes concerning the melting reactions.作者: Ointment 時間: 2025-3-25 08:05 作者: Incorruptible 時間: 2025-3-25 12:30
The Setting of the Ballachulish Intrusive Igneous Complex in the Scottish Highlandsc relations of intrusion, and on the broad history of development of the aureole rocks prior to contact metamorphism. Clearly these features are relevant to models of pressure-temperature-time relationships in the intrusive complex and its aureole, and to examining kinetic controls on the crystallization of the magmatic and metamorphic rocks.作者: Instantaneous 時間: 2025-3-25 19:29 作者: Incorporate 時間: 2025-3-25 20:47 作者: conjunctiva 時間: 2025-3-26 00:39
Field Relations and Petrography of Partially Melted Pelitic and Semi-Pelitic Rockstion, and their implications for the rheological and crystallization behaviour of the melts. The reader is referred to Pattison and Harte (1985, 1988; Sect. 8.5, this Vol.) for notes concerning the melting reactions.作者: finale 時間: 2025-3-26 08:15 作者: paragon 時間: 2025-3-26 12:32 作者: 是他笨 時間: 2025-3-26 13:00
Microtextures and Reaction Mechanisms of Carbonate Rocks: A Comparison Between the Thermoaureoles of heating rates dependent on the distance from the contact. The comparison of the microtextures in these two aureoles, which formed under different pressure conditions, permits the development of a more general theory of the evolution of microtextures during heating. The aim of this chapter is to wor作者: ANTE 時間: 2025-3-26 20:04
Book 1991ds on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera- tures and geologica作者: Morsel 時間: 2025-3-26 23:28
also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera- tures and geologica978-3-642-76147-8978-3-642-76145-4作者: gruelling 時間: 2025-3-27 05:04 作者: 擦試不掉 時間: 2025-3-27 06:56 作者: SOW 時間: 2025-3-27 10:56 作者: Stress 時間: 2025-3-27 15:57
https://doi.org/10.1007/978-94-009-3569-3Clastic minerals of the Appin Quartzite are: ca. 85 vol % quartz, ca. 15% alkali feldspars, heavy minerals (zircone, rutile — partly formed from titanomagnetite during diagenesis, and apatite and tourmaline as very rare exceptions.作者: Pander 時間: 2025-3-27 21:46 作者: SAGE 時間: 2025-3-28 01:10
Florencia Riegelhaupt,Roberto Luis CarrascoOxygen isotope fractionation between coexisting minerals may indicate equilibrium or disequilibrium, provided the temperature of formation is known. Depending on the time of blocking of specific .O/.O ratios, the fractionations contain information on:作者: 頂點 時間: 2025-3-28 05:46 作者: Narrative 時間: 2025-3-28 09:48 作者: Hemodialysis 時間: 2025-3-28 10:55 作者: 細絲 時間: 2025-3-28 18:27 作者: tangle 時間: 2025-3-28 19:07 作者: 吞沒 時間: 2025-3-28 23:08
Detrital Quartz and K-Feldspar in Quartzites as Indicators of Oxygen Isotope Exchange KineticsOxygen isotope fractionation between coexisting minerals may indicate equilibrium or disequilibrium, provided the temperature of formation is known. Depending on the time of blocking of specific .O/.O ratios, the fractionations contain information on:作者: 抱狗不敢前 時間: 2025-3-29 04:58
https://doi.org/10.1007/978-3-642-76145-4Metamorphose; chemistry; formation; geochemistry; geology; metamorphism; mineral; modelling; petrography作者: myelography 時間: 2025-3-29 09:00
Heather Froehlich M.D.,Jose A. Plaza M.D.of the Dalradian Supergroup in the Scottish Highlands (Fig. 1.1). For those who are unfamiliar with the Scottish Highlands, the purpose of this chapter is to give some background to the nature of the Caledonian orogeny in Scotland, the Dalradian Supergroup and the late Caledonian granitoids. The aim作者: 廣告 時間: 2025-3-29 11:58 作者: 人充滿活力 時間: 2025-3-29 16:58
https://doi.org/10.1007/978-3-540-39972-8dization (Sect. 4.1.3). A section on solidus temperatures and the granite system (Sect. 4.1.4) introduces several condensed paragraphs on mineral chemistry, phase relationships and geothermometry (Sect. 4.2; see Weiss and Troll 1989 for further details). The implications for fluid activity and the o作者: libertine 時間: 2025-3-29 20:45 作者: freight 時間: 2025-3-30 01:25
https://doi.org/10.1007/978-3-319-21933-2pelitic rocks in the Ballachulish aureole. Two schematic petrogenetic grids are derived: the first is for mineral assemblages below the onset of partial melting, which define the mapped isograds in Maps 1 and 2 and Figure. 8.1; and the second is for high-grade mineral assemblages which occur sporadi作者: 祝賀 時間: 2025-3-30 04:41
https://doi.org/10.1007/978-3-642-18979-1o the intrusive complex (within Zone V of Pattison and Harte 1985, and Chap. 8, this Vol.). In this chapter we summarize that evidence as seen both in the field and under the optical microscope. We endeavour in our presentation to largely keep description and interpretation in separate sub-sections,作者: thrombosis 時間: 2025-3-30 12:16
Alfredo Pasquarello,Antonio Quattropanireole, so the record of progressive metamorphism is incomplete. The outermost thermometamorphic reaction observed in the aureole leads to the appearance of talc + calcite in siliceous dolomites and impure limestones. In the inner aureole from the point where both forsterite and diopside are formed, 作者: congenial 時間: 2025-3-30 12:48
Charge Radii of Neutron Deficient Mercury, progress are based primarily on experimental results and theoretical calculations (Fisher 1978; Walther and Wood 1984; Rubie and Thompson 1985; Lasaga 1986; Ridley and Thompson 1986). Field-related studies are mainly concerned with the formation of reaction bands (Vidale 1969; Fisher 1970; Joesten 作者: resuscitation 時間: 2025-3-30 18:30 作者: Kernel 時間: 2025-3-31 00:24
978-3-642-76147-8Springer-Verlag Berlin Heidelberg 1991
