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科技导报
| 研究论文 2015, 33(24): 46-51
渤东凹陷南部PL14区T20界面厘定及特征
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黄胜兵, 吴克强, 陈少平, 张洋
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Determination and characterization of T20 sequence boundary in PL14 in the south of Bodong sag
Affiliations
出版时间: 2015-12-28
doi: 10.3981/j.issn.1000-7857.2015.24.008
文章导航
渤东凹陷南部地区油气资源丰富,但多年勘探一直未获重大发现,其中该区新近系与古近系地层分界面T20 的认识不清可能是制约该区油气发现的一个重要因素。本文采用区域控制、单井解析、分类对比的研究思路,综合利用钻井、地震资料,对研究区T20 界面进行了重新厘定和界面特征的对比分析。从古生物、岩性组合旋回变化、地层接触关系等方面,认为应将研究区T20 界面整体上调至一套振幅较弱的波组之中,钻井上该界面上下古生物种群及数量发生突变,并位于一套进积型准层序组的顶面,地层接触关系表现为顶超特征。研究区T20 界面地震反射特征与区域上其他地区存在明显差异,界面上、下地层的岩性、岩相不同于邻区是造成T20 界面地震反射特征差异的重要原因。
古生物特征
/
岩性组合
/
准层序组
/
渤东凹陷
The south of Bodong sag is abundant in oil and gas resources, but its exploration lacks significant breakthrough, which might be due to unclear understanding of T20, the interface of neogene and paleogene strata. This paper determined and characterized the T20 sequence boundary applying regional control, single well analysis, classification and comparison, combined with seismic and logging data. The results show that the T20 sequence boundary should be raised to a set of weak amplitude wave group according to ancient biological, lithologic composition and stratigraphic contact relationship. The surface boundary was characterized by toplap, and located at the top of retrogradational parasequence set; meanwhile, ancient biological population and quantity were changed between the upper and lower strata. The surface characteristics were different from that of the other areas because of the difference in lithology and lithofacies between the upper and lower strata of the T20 sequence boundary.
paleontological characteristics
/
lithologic composition
/
parasequence set
/
Bodong sag
黄胜兵, 吴克强, 陈少平, 张洋.
渤东凹陷南部PL14区T20界面厘定及特征.
科技导报,
2015
, 33
(24)
: 46
-51
.
DOI: 10.3981/j.issn.1000-7857.2015.24.008
HUANG Shengbing, WU Keqiang, CHEN Shaoping, ZHANG Yang.
Determination and characterization of T20 sequence boundary in PL14 in the south of Bodong sag[J].
Science & Technology Review ,
2015
, 33
(24)
: 46
-51
.
DOI: 10.3981/j.issn.1000-7857.2015.24.008
2015年第33卷第24期
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文章信息
doi: 10.3981/j.issn.1000-7857.2015.24.008
接收时间：2015-03-23
首发时间：2016-01-07
出版时间：2015-12-28
收稿日期：2015-03-23
修回日期：2015-08-24
https://castjournals.cast.org.cn/joweb/kjdb/CN/10.3981/j.issn.1000-7857.2015.24.008
引用本文
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2种不同金属材料的力学参数
科 属数 种数 占总种数比例 属 种数 占总种数比例 鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78 小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39 多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39 红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87 小菇属 Mycena 11 5.26 光柄菇属 Pluteus 5 2.39 红菇属 Russula 17 8.13 栓菌属 Trametes 5 2.39
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