Embolism
发表于 2025-3-21 18:10:32
书目名称Geology and Water影响因子(影响力)<br> http://figure.impactfactor.cn/if/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water影响因子(影响力)学科排名<br> http://figure.impactfactor.cn/ifr/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water网络公开度<br> http://figure.impactfactor.cn/at/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water网络公开度学科排名<br> http://figure.impactfactor.cn/atr/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water被引频次<br> http://figure.impactfactor.cn/tc/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water被引频次学科排名<br> http://figure.impactfactor.cn/tcr/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water年度引用<br> http://figure.impactfactor.cn/ii/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water年度引用学科排名<br> http://figure.impactfactor.cn/iir/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water读者反馈<br> http://figure.impactfactor.cn/5y/?ISSN=BK0383383<br><br> <br><br>书目名称Geology and Water读者反馈学科排名<br> http://figure.impactfactor.cn/5yr/?ISSN=BK0383383<br><br> <br><br>
范例
发表于 2025-3-21 22:40:01
Pore Water and Sliding,res. On the other hand, if the block slides down a slope under the force of gravity, the previous difficulty is replaced by two others: the coefficient of friction of rock on rock suggests that an angle of about 30° would be required for gravitational sliding — and that also implies a vertical relie
Pseudoephedrine
发表于 2025-3-22 02:46:06
http://reply.papertrans.cn/39/3834/383383/383383_3.png
脱水
发表于 2025-3-22 04:52:42
http://reply.papertrans.cn/39/3834/383383/383383_4.png
Inculcate
发表于 2025-3-22 11:28:40
http://reply.papertrans.cn/39/3834/383383/383383_5.png
fastness
发表于 2025-3-22 15:14:45
http://reply.papertrans.cn/39/3834/383383/383383_6.png
fastness
发表于 2025-3-22 19:16:11
http://reply.papertrans.cn/39/3834/383383/383383_7.png
Middle-Ear
发表于 2025-3-23 00:40:40
http://reply.papertrans.cn/39/3834/383383/383383_8.png
弯弯曲曲
发表于 2025-3-23 04:36:01
http://reply.papertrans.cn/39/3834/383383/383383_9.png
表否定
发表于 2025-3-23 07:30:59
Role of Pore Water in Deformation of Sedimentary Basins, that important deformation occurs in sedimentary basins while they are accumulating sediment on a subsiding sedimentary column — particularly in the terminal regressive sequence. The regressive sequence itself is due to a neighbouring orogeny outside the sedimentary basin: the creation of mountains