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1)  YPC residential area
扬子石化生活区
1.
This article introduces the major content of reconstruction principle and solution for YPC residential area through analyzing the existing problems.
本文通过对扬子石化生活区当前存在问题的分析,提出了对其改造原则和改造方案的主要内容,对社会上同类既有建筑住宅小区改造、提高人们生活条件、改善居住环境、节能环保,提供了一定的参考。
2)  YPC
扬子石化
1.
This article illuminates the importence of cultivating and advancing the core competence of YPC and presents some important measures on how to do this on the analysis of the environment of YPC.
本文通过对扬子石化生产经营环境和现有核心竞争力现状的分析,说明了培育和提升扬子石化核心竞争力的重要意义,提出了培育和提升扬子石化核心竞争力的对策措施,从而为企业实施基于核心竞争力基础上的发展战略提供思路。
3)  Lower Yangtze Area
下扬子区
1.
Sequence stratigraphic division of the Sinian-Middle Triassic marine strata in the Lower Yangtze area of the Jiangsu-Anhui zone;
苏皖下扬子区震旦纪—中三叠世海相层序地层
2.
Discussion on tectonopalaeogeography of Lower Yangtze Area during the Caledonian Period;
下扬子区加里东期构造古地理问题
3.
Thermo-tectonic history of the Lower Yangtze area since Late Cretaceous:evidence from apatite fission track analysis of sandstones from Pukou Formation
苏皖下扬子区晚白垩世以来的构造—热历史:浦口组砂岩磷灰石裂变径迹证据
4)  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。
5)  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。
6)  middle Yangtze area
中扬子区
1.
Cambrian sequence stratigraphy of the middle Yangtze area;
中扬子区寒武纪层序地层研究
补充资料:颜子生活
1.指蹩脚活儿。
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