DUBIT
发表于 2025-3-21 18:28:21
书目名称Evolution of Geological Structures in Micro- to Macro-scales影响因子(影响力)<br> http://impactfactor.cn/2024/if/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales影响因子(影响力)学科排名<br> http://impactfactor.cn/2024/ifr/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales网络公开度<br> http://impactfactor.cn/2024/at/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales网络公开度学科排名<br> http://impactfactor.cn/2024/atr/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales被引频次<br> http://impactfactor.cn/2024/tc/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales被引频次学科排名<br> http://impactfactor.cn/2024/tcr/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales年度引用<br> http://impactfactor.cn/2024/ii/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales年度引用学科排名<br> http://impactfactor.cn/2024/iir/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales读者反馈<br> http://impactfactor.cn/2024/5y/?ISSN=BK0317728<br><br> <br><br>书目名称Evolution of Geological Structures in Micro- to Macro-scales读者反馈学科排名<br> http://impactfactor.cn/2024/5yr/?ISSN=BK0317728<br><br> <br><br>
爱社交
发表于 2025-3-21 22:29:51
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没花的是打扰
发表于 2025-3-22 00:23:15
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nettle
发表于 2025-3-22 05:23:40
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描绘
发表于 2025-3-22 12:23:01
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Acclaim
发表于 2025-3-22 13:21:26
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Acclaim
发表于 2025-3-22 19:06:30
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合同
发表于 2025-3-23 00:05:50
Overthrust shear in mountain buildingformation is needed. This is the result of an analysis of a comprehensive data set, comprising fold axial plane and cleavage orientations, and finite and incremental strain. There is a tendency for the strain to be concentrated at the nappe boundaries. The orientation of the finite strain stretching
异端邪说2
发表于 2025-3-23 01:49:56
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无可非议
发表于 2025-3-23 06:07:17
Practical analysis of general shear zones using the porphyroclast hyperbolic distribution method: An76), among others. In general shear zones, rigid ellipsoidal grains may rotate either forwards (with the sense of shear) or backwards (counter to the sense of shear) according to their axial ratios and orientations. Grains of a critical shape have their forward motion exactly countered by backward m