Grant 发表于 2025-3-21 18:13:28
书目名称Equilibrium and Kinetics in Contact Metamorphism影响因子(影响力)<br> http://impactfactor.cn/if/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism影响因子(影响力)学科排名<br> http://impactfactor.cn/ifr/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism网络公开度<br> http://impactfactor.cn/at/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism网络公开度学科排名<br> http://impactfactor.cn/atr/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism被引频次<br> http://impactfactor.cn/tc/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism被引频次学科排名<br> http://impactfactor.cn/tcr/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism年度引用<br> http://impactfactor.cn/ii/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism年度引用学科排名<br> http://impactfactor.cn/iir/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism读者反馈<br> http://impactfactor.cn/5y/?ISSN=BK0313496<br><br> <br><br>书目名称Equilibrium and Kinetics in Contact Metamorphism读者反馈学科排名<br> http://impactfactor.cn/5yr/?ISSN=BK0313496<br><br> <br><br>GLIB 发表于 2025-3-21 21:06:35
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浸软 发表于 2025-3-22 02:52:31
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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 graniticOpponent 发表于 2025-3-22 10:58:05
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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.