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1)  Yanghukou coal Mine
羊虎沟
1.
Taiyuan Formation of the Late Carboniferous Epoch was mainly coal bearing strata of theYanghukou coal Mine,The coal─bearing of the Taiyuan formation consists of three cycles oflithofacies.
晚石炭世太原组是羊虎沟煤产地主要含煤岩系,由三个沉积旋回组成。
2)  Yanghugou Form ation
羊虎沟组
1.
About 98 speciesoffossilspores and pollen referred to 55 genera from the Upper Car- boniferous Yanghugou Form ation in Zhongw ei, Ningxia have been studied.
研究了宁夏中卫下河沿上石炭统羊虎沟组孢子花粉化石55 属98 种,建立了两个孢粉组合带,即Laevigatosporites m edius-Cyclogranisporites aureus (MA)带和Torispora securis-Punc-tatisporiteshians(SH)带,其地质时代分别相当于维斯发A-B期和维斯发C-D期。
3)  Dahu gully
打虎沟
1.
the debris flow in Dahu gully is on the east part of Yuexi County,it is 3 km long and the drainage area is only 1.
打虎沟泥石流位于越西县城,发育于越西县城以西,由西向东长约3 km,流域面积约1。
4)  Hupiwan gully
虎皮弯沟
5)  Huyu furrow
虎峪沟
1.
The formation condition and prevention & cure of Xi mount Huyu furrow mud-rock flow in Taiyuan city;
太原市西山虎峪沟泥石流形成条件及防治
6)  Daohugou
道虎沟
1.
Zircon U-Pb Age and Geochemistry of the Daohugou Volcanic Rocks in Ningcheng Area, Inner Mongolia;
内蒙宁城道虎沟火山岩的U-Pb年代学及地球化学研究
2.
The discovery of Pseudotribos robustus not only strongly supports the hypotheses of"tribosphenic molar could have undergone convergent evolution",but also suggests that the Daohugou Biota is Middle Jurassic in age.
粗壮假碾磨齿兽的发现有力地支持了哺乳动物中"三磨楔齿形臼齿趋同演化"的假设,并再一次以直接的化石证据表明内蒙古宁城道虎沟地区含蜀兽类化石地层的时代为中侏罗世。
补充资料:虎皮羊质
1.语本汉扬雄《法言.吾子》:"羊质而虎皮。"比喻外强中干。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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