Weber-test 发表于 2025-3-21 18:08:35
书目名称Caves and Karst of the Greenbrier Valley in West Virginia影响因子(影响力)<br> http://impactfactor.cn/2024/if/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia影响因子(影响力)学科排名<br> http://impactfactor.cn/2024/ifr/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia网络公开度<br> http://impactfactor.cn/2024/at/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia网络公开度学科排名<br> http://impactfactor.cn/2024/atr/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia被引频次<br> http://impactfactor.cn/2024/tc/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia被引频次学科排名<br> http://impactfactor.cn/2024/tcr/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia年度引用<br> http://impactfactor.cn/2024/ii/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia年度引用学科排名<br> http://impactfactor.cn/2024/iir/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia读者反馈<br> http://impactfactor.cn/2024/5y/?ISSN=BK0222682<br><br> <br><br>书目名称Caves and Karst of the Greenbrier Valley in West Virginia读者反馈学科排名<br> http://impactfactor.cn/2024/5yr/?ISSN=BK0222682<br><br> <br><br>Homocystinuria 发表于 2025-3-21 23:50:31
Entscheidungsverhalten im Feld,bsurface either east to Stamping Creek springs or southwest to Locust Spring. However, few parts of the underground are accessible to observation. The caves of the Little Levels are of intermediate size, one to two miles, and many carry active streams which allow some interpretation of the eastern and western edges, but not the central portion.可行 发表于 2025-3-22 03:03:00
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http://reply.papertrans.cn/23/2227/222682/222682_9.pngcritic 发表于 2025-3-23 06:06:18
The Swago Creek Basin,epresented by Barnes Pit, Tub Cave, and the Carpenters-Swago System. The Carpenter-Swago System has 3.1 miles of surveyed passage, and it is strongly controlled by a N60°E fracture system. Extensive stream tracing in the basin reveals details of drainage pattern which is strongly controlled by the shaly Taggard Formation.