外表读作
发表于 2025-3-25 06:55:44
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.
Ointment
发表于 2025-3-25 08:05:04
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Incorruptible
发表于 2025-3-25 12:30:58
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.
Instantaneous
发表于 2025-3-25 19:29:18
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Incorporate
发表于 2025-3-25 20:47:58
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conjunctiva
发表于 2025-3-26 00:39:51
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.
finale
发表于 2025-3-26 08:15:26
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paragon
发表于 2025-3-26 12:32:23
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是他笨
发表于 2025-3-26 13:00:25
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
ANTE
发表于 2025-3-26 20:04:32
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