1) 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。
2) Shiwanshan Basin
十万山盆地
1.
Shiwanshan basin has a Mesozoic to Cenozoic continental sedimentary cover lies over a basement of marine-facies Indosinian deformation.
十万山盆地是在印支期海相沉积基底上发育的中新生界陆相沉积盆地。
3) Yunkai Dashan-Shiwan Dashan area
云开大山-十万大山地区
4) 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。
5) 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。
6) 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
补充资料：十万大山
广西壮族自治区西南部重要气候分界线。山脉呈东北-西南走向,西南伸入越南。长170多公里，宽15～30公里。山体海拔千米左右，主峰莳良岭1462米，是桂南最高点。十万大山区是中生代以来凹陷构造的负单位。中生代红色岩系（砂岩、页岩、砾岩）沉积厚度大，分布广，第三纪以来褶皱断裂上升，成为广西最年轻的褶皱山脉。山势南高北低，南部由1200～1400米的山脊组成十万大山主轴，地势向北逐渐降低，依次出现850米、700米、550米、400米等数列单斜山地及丘陵面。 河流多为顺坡面发育而向北流，属郁江水系。由于多列单斜地形的影响，河流多沿错动的断裂谷地及两单斜山地之间发育,河床曲折急剧转弯与平直相间,多险滩。山地南侧河流短小，独流入海。十万大山南坡的防城县，面临热带海洋,降水丰富,那梭乡年降水量达3700毫米，是广西降水最多之地。北面的上思、宁明，处于背风坡"雨影"地带，雨量较少。与那梭直线距离约50公里的上思县城，年降水量1119毫米，只有那梭的30％。十万大山南麓适宜发展热带作物。热带常绿季雨林发育甚佳，热带树种繁多，主要有窄叶坡垒、乌榄、白榄、海南风吹楠、桄榔、肉实树、红山梅、鱼尾葵等。十万大山有锰、锑、磷、云母、钛等矿产，锰、钛已开采，远销国内外。
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