1) basin in the form of passageway
通道式盆地
1.
Fenghui is a basin in the form of passageway.
丰惠盆地乃通道式盆地 ,在晋室南移、宋室渡江后 ,不少名门望族移居丰惠 ,构成深厚的家族渊源 ;丰惠人沐浴在吴越文化中 ,勤诵读 ,尊师友 ;相对落后的经济又促使丰惠人走出丰惠 ,在广阔天地中锤炼自己。
2) the Yitong Basin
伊通盆地
1.
Lots of subaqueous gravity flow sedimentary bodies were developed in the Eocene strata of Chaluhe Fault Depression,the Yitong Basin.
伊通盆地岔路河断陷始新统中发育大量水下重力流沉积,根据重力流发育位置及沉积特征,可划分为浅水浊流沉积、深水浊流沉积、水下滑塌沉积和水下泥石流沉积4种类型。
2.
The Caluhe Depression of the Yitong Basin is a extension rift basin,due to the complex tectonics,particular morphology,sedimentary source from several directions,several depocenter and subsidence center and the rapid facies transition,there is much difficulty in the stratigraphic division and correlation.
伊通盆地岔路河断陷属于伸展断陷盆地,由于其复杂的构造作用、独特的几何形态、多物源供应、具多个沉积沉降中心以及侧向相变快的特点,给地层划分和对比带来了很大的困难。
3) Yitong basin
伊通盆地
1.
Characteristics and Hydrocarbon Generation-Expulsion Histories of Source Rocks in Moliqing Rift of Yitong Basin;
伊通盆地莫里青断陷烃源岩特征及生排烃史
2.
Diagenesis of reservoir of the Shuangyang Formation of Paleogene in Moliqing Faulted Depression of Yitong Basin, Jilin Province;
吉林伊通盆地莫里青断陷古近系双阳组储层成岩作用研究
3.
Study of Eocene lithologic traps in Chaluhe fault depression of Yitong Basin;
伊通盆地岔路河断陷始新统岩性圈闭研究
4) suitable of city
昭通盆地
5) Tunka basin
通京盆地
1.
Sunjardy volcano in Tunka basin in the Southwestern of Baikal rift belt is composed of chrysolite,labradorstein-andesine,salite and volcanic glasses.
位于贝加尔裂谷带西南端通京盆地的尚加泰火山玄武岩由高拉长石—中长石、贵橄榄石、次透辉石、火山玻璃组成,据对S iO2与全碱(N a2O+K2O)的关系判断,均为碱性橄榄玄武岩,微量元素、稀土元素分布型式与板内碱性玄武岩一致,推测原始岩浆来源于上地幔距地表200 km~250 km深度处,在距地表约40 km处即莫霍面附近开始冷却结晶,该火山活动区可能成因于异常地幔凸起中的物质-能量流沿着断裂在通京盆地内的上升。
6) Datong
大通盆地
1.
Sedimentary systems and Coal accumlation Characters of Dissecting Datong Basin;
大通盆地沉积体系与聚煤特征
补充资料：多通道电子风速计(见转杯式风速表)
多通道电子风速计(见转杯式风速表)
爹豁笔戮翁ng’粗转杯式风速表。
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