1) Upper Yangtze Region
上扬子地区
1.
Lower Cambrian Shale Gas Resource Potential in Upper Yangtze Region
上扬子地区下寒武统页岩气资源潜力
2.
By using of the geological data,gas show in drilling and geochemical information from the Lower Cambrian black shale in Qiongzhusi formation in the Upper Yangtze region,this paper analyzed the accumulation condition of shale gas reservoirs.
利用中国上扬子地区下寒武统筇竹寺组黑色页岩的地质、钻井气显示以及有关地化分析数据,剖析了该区页岩气藏形成地质条件,认为上扬子区下寒武统筇竹寺组黑色页岩发育且区域分布稳定,并呈现出川南、黔北及湘鄂西3个与"海湾体系"密切相关的"优质源岩"分布区,是页岩气成藏最有利的地区;威远及黔西北毕节—大方一带在勘探震旦系灯影组气藏过程中,钻至下寒武统筇竹寺组页岩中普遍见气侵、井涌等不同级别的气显示,部分黑色页岩层段密闭取心测试含有低—中等商业性吸附气含量(0。
2) Middle and Upper Yangtze region
中上扬子地区
1.
Lithofacies Palaeogeography of the Meishucun Age in the Middle and Upper Yangtze Region
中上扬子地区早寒武世梅树村期岩相古地理
2.
With the development of research and exploration,the dominance of marine oil and gas exploration is overhanging in Middle and Upper Yangtze region.
随着研究的深入和勘探力度的加大,中上扬子地区海相碳酸盐岩油气勘探的优势日显突出。
3) Upper Yangtze Region
上扬子区
1.
Sequence stratigraphic framework and its palaeogeographic setting for the Loushanguan Group dolostones of Cambrian in Upper Yangtze Region;
上扬子区寒武系娄山关群白云岩层序地层格架及其古地理背景
2.
This genus is widespread in the Upper Yangtze region Silurian, especially in the Ningqiang Formation (middle-upper Telychian)of southern Shaanxi and northern Sichuan, the Daluzhai Formation (middle-upper Telychian), northeastern Yunnan and the Shamao Formation, western Hube.
该属在我国上扬子区广泛分布于上兰多维列统(Llandovery)特列奇阶(Telychian)中,主要产自川北、陕南的宁强组、云南大关的大路寨组(中、上Telychian阶))、湖北长阳的纱帽组及四川朝天的王家湾组(下特列奇阶)。
3.
The Lower Silurian (Llandovery) rugose coral assemblage zones of Upper Yangtze region is reviewed based on the study of rugose coral fauna succession and sequence stratigraphy.
根据动物群演替和层序地层的研究，厘定上扬子区下志留统（Ｌｌａｎｄｏｖｅｒｙ）四射珊瑚组合带序列：（１）香树园组ＤｉｎｏｐｈｙｌｕｍＲｈａｂｄｏｃｙｃｌｕｓ组合带，时限为Ａｅｒｏｎｉａｎ期；（２）雷家屯组下部ＳｔａｕｒｉａＢｒｉａｎｔｅｌａｓｍａ组合带；（３）雷家屯组上部ＭａｉｋｏｔｉａＫｏｄｏｎｏｐｈｙｌｕｍ组合带，它们对应于Ｔｅｌｙｃｈｉａｎ早期；（４）宁强组ＧｙａｌｏｐｈｙｌｏｉｄｅｓＩｄｉｏｐｈｙｌｕｍ组合带，相当于Ｔｅｌｙｃｈｉａｎ晚期。
4) sequence-stratigraphic framework
上扬子区
1.
This stratigraphic succession represents a complex sequence-stratigraphic framework.
上扬子区,特别是贵州及其邻区的寒武系发育完整,是一套从黑色页岩系到碳酸盐岩的地层序列,该序列构成一个复杂而有序的层序地层格架。
5) the Upper-Yangtze region
上扬子区
1.
In the Upper-Yangtze region,especially in Guizhou Province and its adjacent areas,the Lower Cambrian is well developed and is marked by a succession from black shale to carbonate rocks.
上扬子区特别是贵州及邻区的下寒武统发育完整,是一套从黑色页岩系到碳酸盐岩的地层序列,该序列构成一个复杂而有序的层序地层格架。
2.
The Sinian System in the Upper-Yangtze region contains the Doushantuo Fm.
上扬子区的震旦系包括陡山沱组和灯影组,前者包含较多的黑色页岩,而后者则以大套白云岩为特征。
3.
The Early Palaeozoic strata of the upper-Yangtze region are fully developed in Guizhou Province and its adjacent areas.
上扬子区下古生界在贵州及其邻区发育较为完整。
6) Yangtze area
扬子地区
1.
Lithofacies paleogeography and petroleum geology of the Silurian in Yangtze area;
扬子地区志留纪岩相古地理与石油地质条件研究
2.
Biogenetic barium distribution from the Upper Ordovician to Lower Silurian in the Yangtze area and its significance to paleoproductivity
扬子地区上奥陶—下志留统生物钡特征及其古生产力意义
3.
Through a long-term compaction and geological history, the orlginal porosity and permeability of the marine reservoir rocks in the Lower Yangtze area are greatly decreased, most of them are characterized by low porosity and low permeability.
下扬子地区海相储集岩经过长期压实和地史演化,原生孔隙度和渗透率急剧减小,大部分岩石呈低孔、低渗特征。
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)
太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC
Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
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