1) 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。
2) Yangtze region
扬子地区
1.
Based on the study of the distribution,age and the characteristics of the assemblage of Triassic marine reptiles of the Yangtze region,combined with the analysis of the relations on the diversification of marine reptiles with sea-level changes,volcanic activities and paleogeographical changes,this paper deals with the origin of the Guanling biota and its taphonomic evolution.
在系统介绍扬子地区三叠纪海生爬行动物分布、时代和组合特征基础上,结合海生爬行动物多样性特点及其与海平面变化、火山活动和古地理变化关系的讨论,分析和讨论了关岭生物群的起源与环境演化特点,指出关岭生物群是古生代末期全球生物大绝灭之后,中生代早期海洋生物复苏和生态系统重新建立过程中,在扬子地台三叠纪浅海陆棚环境中的生物与环境协同演化发展所形成的,以海生爬行动物为特色,集多门类脊椎和无脊椎于一体的生物群落。
2.
In the Yangtze region, Ordovician paleogeographic conditions were favorable to the development of source, reservoir and seal rocks in petroleum systems.
扬子地区奥陶纪古地理条件有利于含油气系统生储盖层的发育。
3.
Based on the study of the distribution,age and the characteristics of the assemblage of Triassic marine reptiles of the Yangtze region,combined with the analysis of the relations on the diversification of marine reptiles with sea-level changes,volcanic activities and paleogeographical changes,this paper deals with the origin of the Guanling biota and its taphonomic evolution.
在系统介绍扬子地区三叠纪海生爬行动物分布、时代和组合特征基础上,结合海生爬行动物多样性特点及其与海平面变化、火山活动和古地理变化关系的讨论,分析和讨论了关岭生物群的起源与环境演化特点, 指出关岭生物群是古生代末期全球生物大绝灭之后,中生代早期海洋生物复苏和生态系统重新建立过程中,在扬子地台三叠纪浅海陆棚环境中的生物与环境协同演化发展所形成的,以海生爬行动物为特色,集多门类脊椎和无脊椎于一体的生物群落。
3) middle Yangtze region
中扬子地区
1.
Sedimentary characteristics and lithofacies palaeogeography of the Late Sinian and Early Cambrian in middle Yangtze region;
中扬子地区晚震旦世—早寒武世沉积特征及岩相古地理
2.
Transverse distribution of Lower Cambrian hydrocarbon source rocks in the middle Yangtze region and its major control factors
中扬子地区下寒武统烃源岩横向分布及主控因素分析
3.
The Middle Yangtze region is an important site for marine petroleum exploration in South China.
中扬子地区作为南方海相油气勘探的重点战略区块 ,自基底形成至今 ,陆块南北经历了多期造山活动。
4) Lower Yangtze area
下扬子地区
1.
Evolution of Marine Basins and Exploration Direction Estimation of Oil and Gas in Lower Yangtze Areas;
下扬子地区海相盆地演化及油气勘探选区评价
2.
Lower Yangtze area is one of the prior marine blocks of petroleum exploration in South China.
下扬子地区是中国南方海相油气勘探的优选地区,针对中、古生界海相油气勘探提出了“二次生烃,晚期成藏”的部署思路。
3.
Lower Yangtze area is a superimposition basin modified by multiple tectonic movement.
下扬子区是一个经历了多期构造运动改造的叠合盆地,2种构造体制、2个世代盆地造就了下扬子地区复杂的构造格局。
5) Lower Yangtze region
下扬子地区
1.
Mafic volcanic rocks in Longwangshan Formation from the Lishui Bas in of the Lower Yangtze region are composed of high-K calc-alkaline to shosho nitic trachybasalts and basaltic trachyandesites.
下扬子地区溧水盆地晚中生代龙王山组基性火山岩属高钾钙碱性-钾玄岩系列,具有低MgO(3。
2.
Owing to the continent continent collision between the North China and Yangtze plates during the Indosinian early Yanshanian period, the Lower Yangtze region south of the collision belt developed into a foreland deformation belt.
华北板块与扬子板块于印支—早燕山期发生陆—陆碰撞时，使造山带南部的下扬子地区成为前陆变形带。
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