滇东地区有较丰富的煤炭和煤层气资源。
There are abundant coal and seam gas resources in East Yunnan.
目的系统分析滇东泥质基底澄江化石库腕足动物的生活方式。
Aim To infer the life strategies of Early Cambrian brachiopods on muddy substrate from the brachiopods in the Chengjiang fauna of Yunnan, China.
滇东晚二叠世含煤岩系良好的岩性组合，贮藏了丰富的煤层气资源。
The excellent rock assemblage of Late Permian coal -bearing rock series in East Yunnan contains abundant seam gas resources.
在滇东黔西地区，海相和陆相二叠—三叠系界线附近均有界线粘土岩存在。
There exists boundary claystone near the boundary between both the Marine and terrestrial Permian and Triassic in the eastern Yunnan-western Guizhou area.
六盘水市位于贵州西部，地处滇东高原向黔中山原过渡地带，是茶树原生地之一。
Liupanshui city is located in the west Guizhou, at the transition zone of east Yunnan plateau to Guizhou plateau, is one of the primary tea places.
作者就是在上述认识的基础上提出了新看法并对滇东地区的强震活动趋势进行了探讨。
On the basis of the understanding mentioned above, the author has provided a new opinion, and made an exploration to tendency of strong earthquake in North-East Yunnan.
滇东黔西地区煤层气资源丰富，开发煤层气资源，为该区的经济腾飞将起到极大的推动作用。
Coalbed gas resources are very rich in East Yunnan and West Guizhou area. And to develop them can promote the economic prosperity of this area.
在滇东-川西地区的下二叠统中，白云岩发育，并可分两种类型：块状白云岩和斑状白云岩。
In the East yunnan-west Sichuan area, dolostones are well developed and can be divided into two types: massive dolostones and patchy dolostones.
上扬子西部滇东、黔西茅口组之上多为峨眉山玄武岩所覆盖，长期以来人们一直认为两者不存在沉积间断和地层剥蚀。
The Middle Permian Maokou Formation is generally overlain by the Late Permian Emeishan basalts in eastern Yunnan and western Guizhou in the west of the Yangtze platform.
川滇地块东测边界带，由曲江、小江至鲜水河断裂带自南而北现今水平形变量逐渐减小；
Along some eastern boundary belts: Qujiang, Xiaojiang fault belts in the south of Yunnan to Xianshuihe fault belts in northwestern Sichuan, the present horizontal deformation rate decreases.
川滇地块东测边界带，由曲江、小江至鲜水河断裂带自南而北现今水平形变量逐渐减小；
Along some eastern boundary belts: Qujiang, Xiaojiang fault belts in the south of Yunnan to Xianshuihe fault belts in northwestern Sichuan, the present horizontal deformation rate decreases.
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