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1)  Lianyuan coal basin
涟源煤盆地
1.
The Lower Carboniferous Ceshui and Upper Permian Longtan coal series are most important in Southeast China, and can both generate and bear gas greatly in the Lianyuan coal basin, Central Hunan, China.
湘中涟源煤盆地早石炭世测水组、晚二叠世龙潭组煤系是中国东南诸省境内最重要的煤系,具有较大的生气、储气能力。
2)  Lianyuan basin
涟源盆地
1.
Basic features of the Chengbu-Taojiang basement fault along the Lianyuan basin;
城步-桃江断裂在涟源盆地的基本特征
3)  Lianyuan geodome
涟源地穹
4)  Lianyuan
涟源
1.
The Thermal History and Hydrocarbon-generating characteristics of Ceshui and Longtan Coal Series in Lianyuan,Hunan Province;
涟源地区测水组、龙潭组煤热演化史及生烃特征
5)  coal basin
煤盆地
1.
All varions structures formed by crustal stress changed the shape of original coal basin after formation of coal basin.
含煤盆地形成之后,受地应力作用产生的各种构造现象,改变了原始煤盆地的形态,且具有多样性、复杂性。
2.
Exemplified by the Stephanian Cevennes coal basin on the Central Plateau in France, this paper discusses the coal-forming environments in the intermontane faulted basin.
本文以法国中央高原斯蒂芬期(C3)塞文(Cevennes)断陷聚煤盆地为例,据其不同阶段岩相古地理展布特征与早期构造在空间上的配置关系,指出了成煤环境在时间上的演替这一动态过程与盆地的构造活动性之间的内在联系。
3.
On the basis of tectonic evolution in Junggar coal basin and taking coal mineral as "the fossil" and by way of studying the basin formation and tectonic evolution in every stage.
以准噶尔煤盆地的构造演化为依据,以煤矿产为“化石”,通过对煤盆地形成和构造演化各个阶段的研究,确定了准噶尔煤盆地具有前寒武纪的结晶基底。
6)  coal-bearing basin
含煤盆地
1.
Analysis of structural and sedimentary filling evolution of buya coal-bearing basin in Xinjiang
新疆布雅含煤盆地构造及沉积充填演化分析
2.
A series of late Jurassic-early Cretaceous coal-bearing basins have developed in southern Songliao Basin and distributed regularly.
松辽盆地南部发育了一系列晚侏罗世—早白垩世含煤盆地,呈规律性展布。
补充资料:涟上别王秀才
【诗文】:
飘飖经远道,客思满穷秋。浩荡对长涟,君行殊未休。
崎岖山海侧,想像无前俦。何意照乘珠,忽然欲暗投。
东路方箫条,楚歌复悲愁。暮帆使人感,去鸟兼离忧。
行矣当自爱,壮年莫悠悠。余亦从此辞,异乡难久留。
赠言岂终极,慎勿滞沧洲。



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【出处】:
全唐诗:卷211_36
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