| 1. | Evaluation on source rocks in kongdian formation of deep bohai bay basin
渤海湾盆地深层孔店组烃源岩评价 |
| 2. | Primary study on sequence stratigraphy of kongdian formation in dongying - huimin sag
惠民凹陷孔店组层序地层学研究 |
| 3. | Evaluation of source rocks in kongdian formation and analysis of oil sources in weibei sag
潍北凹陷孔店组烃源岩评价及油源分析 |
| 4. | Sedimentary environment of dark mudstone member of kongdian formation from well wang 46 , dongying sag
东营凹陷王46井孔二段暗色泥岩沉积环境 |
| 5. | Fan - delta sedimentation formed under the environment of lake level frequently varying taking the first member of kongdian formation , huanghua depression as an example
以黄骅坳陷枣园油田孔一段沉积为例 |
| 6. | The petrographic and xrd analysis reveals that the reservoir of the upper part of kongdian formation mainly consists of feldspathic and minor amount of lithic sandstone . the feldspar is consisting mainly of na
岩石学与xrd全岩分析表明，孔店组上段砂岩主要为长石砂岩，此外还发育少量岩屑砂岩。 |
| 7. | The general thickening from the southwest towards the northeast and north , combined with increasing of fine clastic to the northeast and north , indicate principle source of the upper kongdian formation from the southwest and south
自南而北地层逐渐加厚、细粒沉积物含量以及地层内部反射结构表明孔店组沉积时期物源来自研究区南部。 |
| 8. | The stratigraphic analysis reveals that the upper part of kongdian formation is characterized by thickness range from 461 - 744 m and average of thickness of 602 . 5 m . the number quantity of sandstone increased to the north and northwest , indicating more sand bodied are found at these directions
地层学分析表明南斜坡主要发育孔店组上段，地层自南向北逐渐增厚，地层厚度一般为461 - 744m ，平均厚602 . 5m 。 |
