1) Darongshan-Shiwandashan
大容山-十万大山
1.
Origin of the Darongshan-Shiwandashan S-type granitoid belt from southeastern Guangxi:geochemical and Sr-Nd-Hf isotopic constraints;
桂东南大容山-十万大山S型花岗岩带的成因:地球化学及Sr-Nd-Hf同位素制约
2) Shiwandashan
十万大山
1.
Carbonate reservoirs prediction with sequence stratigraphy:application in Shiwandashan area;
碳酸盐岩层序地层储层预测——十万大山地区的应用
2.
Study on diagenesis-sequence stratigraphy of Lower-Middle Devonian dolostone in Shiwandashan area, Guangxi, China;
十万大山地区下-中泥盆统白云岩成岩层序地层学研究
3.
Hopea chinensis which belongs one of the second class national protected plants,is only distributed in Shiwandashan in Guangxi.
狭叶坡垒(Hopea chinensis)是国家二级重点保护植物,仅分布于广西十万大山。
3) Shiwandashan Mountain
十万大山
1.
A Composition Analysis of the Butterfly Fauna of Shiwandashan Mountain in Guangxi;
广西十万大山蝶类区系组成的初步研究
2.
The numerical study on characteristics of pteridophyte flora and vertical distribution of Shiwandashan Mountain,Guangxi;
广西十万大山蕨类植物区系特征及垂直分布的数量研究
3.
There are wonderful natural environment in Shiwandashan Mountain, rich in tourism resources, rational development can bring the resources function into full play, and bring benefit to mankind.
十万大山自然环境优越 ,旅游资源丰富 ,合理开发可以充分发挥资源效能 ,造福人民。
4) Darongshan-Shiw andashan granitic belt
大容山-十万大山花岗岩带
5) Yunkai Dashan-Shiwan Dashan area
云开大山-十万大山地区
6) Shiwandashan Basin
十万大山盆地
1.
The evolution of the Shiwandashan Basin in Guangxi and its response to oil and gas resources;
广西十万大山盆地演化过程及油气资源响应
2.
The Tingliang reef palaeopool of the lower Permian Maokou Formation is one of the destroyed oilpools in the Shiwandashan basin of Guangxi province,and its bitumen-bearing reservoir (above 98 meters in the thickness) occurs mainly in the upper part and at the top of the reef body.
广西宁明县亭亮下二叠统茅口组生物礁古油藏,为十万大山盆地已暴露破坏的礁古油藏之一。
3.
The Shiwandashan Basin in Guangxi Province,South China,is a foreland basin developed from Late Triassic to Cretaceous.
十万大山盆地是印支期以来发展起来的中、新生代陆相盆地。
补充资料：六万大山
郁江、南流江分水岭。位于广西壮族自治区南部、东北-西南走向。山体主要由燕山期花岗岩构成，古老变质岩系零星分布在花岗岩山地外围。山脉中脊海拔千米左右，主峰葵扇顶海拔1118米。山体庞大，高峰起伏，山体主峰外围为低山丘陵所围绕。沟谷多沿次级构造线作西北-东南方向发育，横切山地，造成许多与山脉走向相交的岭谷地形。山坡陡峻，多急滩瀑布，水力资源丰富。由于高温多雨，花岗岩地区风化作用强烈，暴流散流地形明显。六万大山区有面积达1.46万多公顷的六万山林场，松杉针叶林和松、杉、楠、椎针阔混交林集中连片，林相郁闭，保护水土作用良好。六万大山山脉向北延伸为大容山。二者原为一条东北-西南走向山脉，因被与其相交的西北-东南走向的石南断层谷地分隔，成为两大山脉，大容山亦为花岗岩侵入而成，大容山主峰梅花顶1276米，为桂东南最高峰。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条