Titlebook: Equilibrium and Kinetics in Contact Metamorphism; The Ballachulish Ign Gerhard Voll,Jutta Töpel,Friedrich Seifert Book 1991 Springer-Verlag

hidebound

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

Euphonious

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

态学

挡泥板

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.

别炫耀

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).

Multiple

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.

粗糙

Tracheotomy

uncertain

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.

overbearing

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).