| 1. | It was developed mostly deep lake facies on the south of basin and coastal - shallow lake facies on the north of basin
此时期盆地南缘主要发育半深湖亚相，盆地北缘则发育滨浅湖亚相。 |
| 2. | From northern and western to southern and eastern , the sedimentary facies transited from fan delta , braided delta to lake facies
由北、西向南、东，沉积相由扇三角洲、辫状河三角洲向湖泊过渡。 |
| 3. | Discovery and study of the early pleistocene river and lake facies stratum in bukedaban area of the western segment in the eastern kunlun mt
东昆仑西段布喀达坂峰地区早更新世河湖相地层的发现及初步研究 |
| 4. | Flat bedding , wavy bedding and vermiglyph were often found in the shallow lake facies , and the log was usually straight or slight dentation
滨浅湖相常发育水平层理、波状层理及虫迹，测井曲线形态较平直，常呈微齿状。 |
| 5. | 3 ) the pingdiquan formation mainly are the deposition of lake and fan - delta , fan - delta developing in the background of the lake facies sedimentary
平地泉组以湖，扇三角洲相沉积为主，扇三角洲的生长是在湖相的背景下进行的。 |
| 6. | The types of sedimentary facies were mainly fan - shaped delta , delta , binshore subaqueous fans , slump turbid fan , lake facies , fluvial facies
该研究区主要发育扇三角洲、三角洲、近岸水下扇、滑塌浊积扇、湖相和河流相沉积。 |
| 7. | Early permian was initial stages of expanding of the lake basin . inside the region of interest , there developed fan delta , braided delta and lake facies
早二叠世是湖盆扩张初期，区内发育扇三角洲相、辫状河三角洲相和湖泊相。 |
| 8. | In the fairly deep lake facies there found abundant bivalve fossils , such as the standard foss il of permian in north xingjiang - tarfaniasp . ,
半深湖相中发现丰富的瓣鳃类动物化石，如北疆地区二叠系标准化石?吐鲁番鳕鱼及介形类等。 |
| 9. | Ostracoda , and so on . in the deep lake facies of niujuanhu and mazhong structural belts , there were also discovered gravity - flow microfacies , which was mainly composed of turbidite in which the slump structure and convolute bedding were often found
马朗凹陷牛圈湖构造带、马中构造带的半深湖相中，发育湖泊重力流微相，典型的表现为浊积岩的发育，其中可见到重力滑塌构造及包卷层理等。 |
| 10. | At the beginning of tiaohu period , the lake basin shrank , and the water became shallow . braided river facies and braided delta facies were found on both side of the basin , and deep lake facies disappeared , and shallow lake facies was only found in the southern of tiaohu seg and central part of malang seg
从中二叠世条湖期开始，湖盆发生萎缩，水体变浅，盆地南北两侧出现辫状河及辫状河三角洲相沉积，半深湖相消失，仅在条湖凹陷南缘及马朗凹陷中部残余滨浅湖相沉积。 |
