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发表于 2025-3-21 16:47:16
书目名称Origins of Igneous Layering影响因子(影响力)<br> http://figure.impactfactor.cn/if/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering影响因子(影响力)学科排名<br> http://figure.impactfactor.cn/ifr/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering网络公开度<br> http://figure.impactfactor.cn/at/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering网络公开度学科排名<br> http://figure.impactfactor.cn/atr/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering被引频次<br> http://figure.impactfactor.cn/tc/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering被引频次学科排名<br> http://figure.impactfactor.cn/tcr/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering年度引用<br> http://figure.impactfactor.cn/ii/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering年度引用学科排名<br> http://figure.impactfactor.cn/iir/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering读者反馈<br> http://figure.impactfactor.cn/5y/?ISSN=BK0704643<br><br> <br><br>书目名称Origins of Igneous Layering读者反馈学科排名<br> http://figure.impactfactor.cn/5yr/?ISSN=BK0704643<br><br> <br><br>
Proponent
发表于 2025-3-21 21:20:56
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ROOF
发表于 2025-3-22 04:07:14
1389-2185 ro-syenite transition 41 5. The layered series 43 5. 1 General relationships 43 5. 2 Granular syenites 43 5. 2. 1 Structure and cryptic variation 43 5. 2. 2 Ori978-90-481-8435-4978-94-017-2509-5Series ISSN 1389-2185
SPURN
发表于 2025-3-22 05:44:20
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Lacerate
发表于 2025-3-22 09:50:56
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Abominate
发表于 2025-3-22 13:14:17
A. J. Naldrett,G. Cameron,G. von Gruenewaldt,M. R. Sharpe
burnish
发表于 2025-3-22 19:37:23
Layering in the Ilimaussaq Alkaline Intrusion, South Greenland,ering and macrorhythmic layering. The mineralogy of the kakortokite series is described, and theories of formation of the layering reviewed. Crystallisation probably took place in a stagnant bottom layer, and the layering is considered to be caused by different nucleation and growth maxima, in relat
Jejune
发表于 2025-3-22 23:55:40
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全能
发表于 2025-3-23 04:34:49
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招募
发表于 2025-3-23 08:17:03
The Southern Part of the Fongen-Hyllingen Layered Mafic Complex, Norway: Emplacement and Crystallize wall, varying over 7km from Fo.:An. to Fo.:An.. The apparent angle between cryptic and modal layering is usually less than 20°. The start of the major regression, reflecting the influx of fresh magma at the floor of the chamber, is concordant with modal layering which implies that modal layering r