1.
The deep-water in situ deposits and deep-water allogene deposits develop flysch rhythmic sequences.
深水原地沉积与异地沉积在剖面上组成了复杂的复理石韵律。
2.
In situ deposits are dark shale with horizontal bedding.
原地沉积为水平层理发育的暗色泥板岩。
3.
The sedimentary microfacies of Taiyuan formation in the Hangjinqi area,the north of Ordos Basin
鄂北杭锦旗地区太原组沉积微相分析
4.
THE EXISTENCE OF A LARGE-SCALE TRIASSIC SEDIMENTARY BASIN IN NORTH CHINA
华北地区大型三叠纪原始沉积盆地的存在
5.
Climatic Change Recorded by Sedimentary in Kunlun Pass Basin of Qinghai-Tibet Plateau;
青藏高原昆仑山垭口盆地沉积记录的气候变化
6.
Study on Deposition Palaeogeography Feature in Late Jurassic, in Southern Tibetan Plateau
青藏高原南部晚侏罗世沉积古地理特征
7.
glacial outwash
【地质】冰水沉积, 冰水漂积
8.
Some thick chaotic deposits appear to be mass flows and talus deposites; others are early insituated dissolution residues.
一些厚的混杂沉积物看来是块状流沉积和山麓堆积物，另一些是早期原地的溶解残余物。
9.
Research on Sedimentary Response to Uplifting of Tibetan Plateau Hinterland and Oil-gas Reservation during the Late Cretaceous-Paleogene Period;
青藏高原腹地晚白垩—古近纪高原隆升的沉积响应与油气后期保存
10.
locate in fault basin or sediment basin among plateaus,have deep and great rupture developing and controlling;
均处断陷盆地或高原山间沉积盆地,有深大断裂发育控制;
11.
SEDIMENTARY PATTERN OF PROTOTYPE BASIN IN THE DEPOSITION PERIOD OF LAIYANG FORMATION AND THE ADVANTAGEOUS AREAS FOR OIL AND GAS EXPLORATION OF JIAOLAI BASIN
胶莱盆地莱阳期原型盆地的沉积格局及有利油气勘探区选择
12.
Sedimentary Characteristics of the Yanqi Prototype Basin in Mesozoic Era and the Determination of the Basin Boundaries
焉耆中生代原型盆地沉积特征与盆地边界的确定
13.
The Sedimentary Facies and Sequence Stratigraphy of Middle-Later Jurassic Epoch in Easten Qiangtang Basin, Qingzang Plateau;
青藏高原羌塘盆地东部中—晚侏罗世沉积相及层序地层分析
14.
The Depositional Evolution and Tertiary Tectonic and Reconstruction of the Cretaceous Proto-type Basin in Liupanshan Basin
六盘山盆地白垩系沉积构造演化及原型盆地研究
15.
Research on Sedimentary System, Reservior Characteristics for Yanchang Formation in Zhenyuan-Jingchuan Field, Ordos Basin
鄂尔多斯盆地镇原—泾川地区延长组沉积体系与储层特征研究
16.
Sedimentary characteristics of shallow water delta of the Lower Permian Taiyuan Formation in Shenmu area,Ordos Basin
鄂尔多斯盆地神木地区下二叠统太原组浅水三角洲沉积特征
17.
Channels generally contain coarser sediment than do the adjacent flood plains.
河床沉积物一般比邻近的泛滥平原沉积物粗些。
18.
Sedimentary evolution of Tangyuan Rift and sedimentary facies of Dalianhe Formation of Eogene
汤原断陷沉积演化及下第三系达连河组沉积相