1.
The Study of Tectonic Evolution of Late Paleozoic Strata in the East of Inner Mongolia;
内蒙古东部地区晚古生代地层构造演化研究
2.
schistose structure
【地质】片状构造, 层状结构
3.
Tectono-stratigraphic Features of the Yanbian Group and Their Geotectonic Implications;
盐边群构造地层特征及其大地构造意义
4.
Paleoproterozoic strata sequence and tectonic setting in southern Jilin Province
吉南地区古元古代地层层序及构造背景
5.
Sequence Stratigraphy and Non-Structural Reservoir of Upper Part of the Third Member of Shahejie Formation in Dawangzhuang Area
大王庄地区沙三上亚段层序地层与非构造油藏
6.
The accumulations are atratigraphic and bear no relation to structure.
聚集作用是地层型的，而与构造无关。
7.
Drilling fluid technology for the upper formation of Qiongkuqiake structure, Tarim
琼库恰克构造带上部地层钻井液技术
8.
The Research of 3D Modeling for Tectonic-Stratigraphic Framework Based on Borehole Data;
基于钻孔资料构造—地层格架三维建模
9.
Tectonic-sequence-based Lithofacies and Paleogeography of Permian in South of China
中国南方二叠纪构造—层序岩相古地理
10.
Late Paleozoic Strata and Tectonic Facies in the Northern Margin of the Eastern Kunlun Orogen and their Tectonic Implications
东昆仑南缘晚古生代地层组合、大地构造相及大地构造意义
11.
SYN-RIFT TECTONIC-SEQUENCE STRATIGRAPHIC CHARACTERISTICS OF THE LOWER CRETACEOUS FORMATIONS IN NORTHEASTERN CHINA
东北区早白垩世同裂谷期构造－层序地层特征
12.
The layer order of ore-hosted strata is normal by structural feature.
根据小构造标志，判定含矿岩系地层为正常层序。
13.
Structural-Sequence Stratigraphy and Depositional System Research of Paleogenein Baxian Depression;
霸县凹陷古近系构造—层序地层与沉积体系研究
14.
Fine Tectonic Interpretation and Reservoir Prediction of Shallow Layer in Shallow Sea of NanPu;
南堡滩海地区浅层精细构造解释及储层预测
15.
SEQUENTIAL STRATIGRAPHIC ANALYSIS OF XINGANLING GROUP AT BEI-14 BLOCK IN SUDEERTE TECTONIC BELT
苏德尔特构造带贝14块兴安岭群层序地层分析
16.
Compression Salt Tectonics and Synkinematic Strata Study in the Middle to Western Kuqa Foreland Basin, Southern Tian Shan
南天山库车前陆盆地中—西段挤压盐构造及同构造沉积地层研究
17.
The characteristics of different structure layers and tectonic implications since late Paleozoic in Kalamaily Area,Xinjiang
新疆卡拉麦里地区晚古生代以来不同构造层特征及大地构造意义
18.
And the places where these plates come up against one another are called faults in the earth's crust.
构造板块挤在一起的地方，就叫做地壳的断层。