六盘山，拦路虎，费用高。
六盘山突齿蟾为中国特有珍稀动物品目之一。
Liupanshan sudden tooth laevis as one of the items rare animals unique to China.
六盘山白垩纪盆地是六盘山内陆叠合盆地的一个单型盆地。
Liupanshan Cretaceous basin is a mono-basin of Liupanshan inland overlapping basin.
从海参1井钻井剖面出发，建立六盘山盆地中新生代层序地层格架。
Starting from the profile of Haishen no. 1 well, this paper establishes the sequential stratigraphic framework of middle Cenozoic in Liupanshan Basin.
磷灰石裂变径迹研究表明，六盘山盆地白垩系地层经历两次埋深加热事件。
Apatite fission track data suggest that the early Cretaceous strata in the Liupanshan basin were subjected to two burial heating events.
六盘山盆地位于河西走廊东南端，处于鄂尔多斯盆地西缘，白垩纪是其主要成盆期。
The Liupanshan Basin. which was mainly formed during the Cretaceous. is located in the southeastern tip of the Hexi Corridor and on the west of the Ordos Basin.
东倚子午岭，北靠羊圈山，西接六盘山，东、西、北三面隆起，中南部低缓，故有“盆地”之称。
Ziwuling East Hill, north mountain sheep pen, Liupanshan west, east, west, north uplift, central and southern low-, it is "basin" of.
基于野外变形分析与断层滑动矢量构造应力场反演，初步确定了六盘山盆地形成与构造演化历史。
Based on the field analysis of deformation and stress field inversion from fault slip data, the formation and tectonic evolution history of the Liupanshan basin has been preliminarily established.
从生态系统响应和游客主观认知的双重视角，对六盘山旅游区旅游步道对人类旅游践踏干扰的响应进行了研究。
From the angles of the response of ecosystem and tourist perceptions, the response of Liupan mountain ecological tourism attraction trails to human being tourism trampling disturbance was studied.
西海原—海原—六盘山断裂带西南侧地块内发育连续成层的壳内低阻层，而其东北侧不存在大范围连续壳内的低阻层。
Southwest to the west Haiyuan-Haiyuan-Liupanshan fault exists continuous layered LR material in crust, while in its northeast side there is no such LR layer in crust.
西海原—海原—六盘山断裂带西南侧地块内发育连续成层的壳内低阻层，而其东北侧不存在大范围连续壳内的低阻层。
Southwest to the west Haiyuan-Haiyuan-Liupanshan fault exists continuous layered LR material in crust, while in its northeast side there is no such LR layer in crust.
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