| 1. | Braided - fan - delta deposit
网状冲积扇三角洲沉积 |
| 2. | Delta deposits of braided river from shahejie formation , lower tertiary in bonan sag
渤南洼陷下第三系沙河街组辫状河三角洲沉积 |
| 3. | Braided stream delta deposit of eogene es102 in haojia - shinan area of dongying depression
史南地区下第三系沙二10辫状河三角洲沉积 |
| 4. | Fan - delta and wave - dorminated delta deposits of the upper - jurassic in songjia depression , liaohe basin
辽河盆地宋家洼陷上侏罗统扇三角洲和浪控三角洲 |
| 5. | Fan delta deposits and relation to hydrocarbon of upper es4 at yong 921 area in dongying depression
山东东营凹陷永921地区沙四上亚段扇三角洲沉积与油气 |
| 6. | Fan delta deposits of sha - 3 and sha - 4 members at oligocene shahejie formation at yong 921 area in the north of dongying depression
东营凹陷北部永921地区渐新世沙三段和沙四段扇三角洲沉积 |
| 7. | Baibao area lies in the middle - south of the basin , delta deposit was belong to the north set of jingbian - wuqi delta and locating at front region
白豹地区位于盆地中南部，三角洲沉积属于北部靖边?吴旗三角洲向西南延伸部分，主要发育三角洲前缘沉积。 |
| 8. | The seawater thereafter withdrawed southward away from the area , and form abundant stream , lake and delta deposit in shanxi stage and the early shihezi stage and stream , lake and bog deposit in the late shihezi stage and shiqianfeng stage
随后，海水向南退出本区，并在山西期、石盒子早期形成广泛的河流、湖泊和三角洲沉积，在石盒子晚期和石千峰期形成河流、湖泊和漫滩沼泽沉积。 |
| 9. | Yanchang 4 + 5 sector to yanchang 3 sector lithofacies palaeogeography pattern was stable , because the constitution background was steady , and the source direction had no change , and supply was abundant . in those sectors the basin development was in lake retreat , and in the period of extinction gradually , and formatted construction delta deposit , but in yanchang 33 period the sedimentary speed were greater than construction speed , showing that overriding river mouth bars were abundant
长4 + 5 ?长3期湖盆发展处于湖退、萎缩逐渐消亡时期，由于构造背景稳定，物源来源方向没有变化，物源供给充分，所以岩相古地理格局基本一致，形成建设性三角洲沉积，但长3 ~ 3期沉积速率大于构造沉降速率，表现为叠置河口砂坝极其发育。 |
