排序方式: 共有7条查询结果,搜索用时 15 毫秒
1
1.
黔西县水西洞主要呈NE-NEE向发育于下三叠统茅草铺组(T_1m)可溶岩层内,由五条主洞及三个洞厅组成,实测长度为10557. 13 m,最低点高程762. 12 m,最高点高程920 m,高差达157. 88 m。洞道形态呈拱形、梯形、三角形等,洞穴次生碳酸钙沉积物充分发育,不同类型的沉积物通常相伴生,部分洞段分布较密集,规模体量较大,多沿层理、节理发育,造型较美观,具有极高的观赏价值和美学价值。冲积物主要为粘土及粉砂。水西洞形成经历了深潜期、渗流期及半悬托期三个阶段,是区域地质构造演化的反映,洞内广泛分布的石笋是了解古气候演变的重要载体,具有较高的科学价值。 相似文献
2.
In this paper, we apply the adiabatic approximation model to the IR absorption of molecules. Expressions of the band shape functions for isothermal and isolated systems are obtained and using Einstein model we discuss the dependence of the band shape functions on temperature, normal coodinate shifts and energy.We also obtain a very simple expression of the correlation function when Svv′< 1 and discuss its effect on the band shape function. 相似文献
3.
4.
5.
In this paper, we apply the adiabatic approximation model to the IR absorption of molecules. Expressions of the band shape functions for isothermal and isolated systems are obtained and using Einstein model we discuss the dependence of the band shape functions on temperature, normal coodinate shifts and energy.We also obtain a very simple expression of the correlation function when Svv ′<1 and discuss its effect on the band shape function. 相似文献
6.
7.
威宁一带尚未有可供开发的洞穴旅游资源报道。对威宁县老干洞进行实地测量并绘制洞穴图,结果显示,老干洞呈NE-SW向发育于下二叠统茅口组(P1m)灰岩中,由1条主洞及4条支洞组成,实测长度为1 038 m,深度为24.67 m。洞穴总共分为三层,二、三层洞穴洞底发育季节性地下河,第一层洞底终年积水。洞道坡降较小,形态呈拱形、三角形、椭圆形、楔形、梯形等,滴石类及流石类洞穴次生化学沉积物发育,冲积物主要为粘土及粉砂。老干洞为一大型洞穴,在适宜的气候、岩性、构造及水文条件下形成,洞穴形成经历了深潜期、渗流期及半悬托期三个阶段,具备一定的开发价值,可整合周边旅游资源综合开发,将带动区域经济发展。 相似文献
1