Miocene foraminifera of Tarim basin, Xinjiang and their geological significance
新疆塔里木盆地中新世有孔虫及其地质意义
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It is shown that the Tarim basin ends at E91 ° longitude and no longer extends toward east.
指出塔里木盆地在E91°附近结束，不再向东延伸。
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吐哈盆地是我国最炎热的地区之一，属极端干旱的温带内陆荒漠气候，其独特的光热资源优势，形成了该地区以葡萄树为主的林果业的特色支柱产业。
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Hengyang Basin which was a typical hilly area in subtropical zone acted as the research subject.
以亚热带丘岗山区的典型区域——衡阳盆地为研究对象,分析了其雨水资源利用的必要性、可行性.
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The interaction of meteoric water-sandstone is an important part of the research of the basin fluid.
大气水 - 砂岩的相互作用是盆地流体研究的重要内容.
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塔里木盆地西南部&西昆仑地区构造电性特征与A型俯冲模式
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Chlorine is highly incompatible during the whole evolution of the eastern Manus basin magmas.
氯在东Manus岩浆中表现为高度不相容的特点。
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Gao 81 surveyprospective area, lies in Northern of West Depression, Liaohe Basin.
高81井区位于辽河盆地西部凹陷北段构造北部, 是具有勘探潜力的新区.
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Comparative Analysis on Basin Water Pollution Control& Huai River with Rhine, Danube River
流域水污染防治的比较研究&淮河与莱茵河、多瑙河
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Dynamic Equation of Grassland Biomass and Study on the Development and Utilization of Hanshan Basin
寒山流域草地生物量动态方程与开发利用研究
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