Deep Crust Structure and Petroleum Potential in Yixian-Beipiao Basin, Liaoning Province一And concurrently produced the mystery with large-area species death in terms of rare animal

Abstract

Abstract: It causes domestic geoscientists' great concern that the abundant biological fossil group of Rehe in western Liaoning was found, especially the dinosaur with feather and rare birds were discovered, with various animals' large-area death but keeping remains intact. The comprehensive study of Dongwuzhumuqinqi- Haicheng-Donggou cross-section indicates that there exists a low-velocity layer (v_p=5.8-6.0km/s) in deep middle-crust of Yixian-Beipiao basin. According to the distribution of Pb isotope discontinuity zone, it is considered that large-sized oil-gas field exists in the deep of this basin. Also, this paper reveals the mystery of concurrent formation of the rare bio-fossils and large- area death of the species.

Key words: Yixian-Beipiao basin, Yixian formation, rare fossil, species extinction, cross section, middle crust, low-velocity layer, isotope discontinuity zone, petroleum potential

CLC Number:

TE111.1

ZHANG Jing-lian. Deep Crust Structure and Petroleum Potential in Yixian-Beipiao Basin, Liaoning Province一And concurrently produced the mystery with large-area species death in terms of rare animal[J]. Xinjiang Petroleum Geology, 2005, 26(4): 445-449.

References

[1] Ji Q,Curie PJ,Norell M A,et al.Two feathered dinosaurs from northeastern China [D].Nature,1998 ,393:753-761.
[2] Chen P J,Dong Z M,Zhen S N,An exceptionally well preserved theropod dinosaur from the Yixian Formatim of China[J].Nature,1998,391: 147-152.
[3] Sun G,DilcherD L,Zheng S L,et d.In search of the first flower: a Jurassic angiosperm,arohaefructus,from Northeast China[J].Science,1998,282:1 692-1 695.
[4] Swisher C C.Cretaceous age of the feathered dinosaurs of Liaoning,China[J].Nature,1999,400:58-61.
[5] Zhang F C,Zhou Z H.A primitive enantiomithine bird and the origin of feathers[J].Science ,2000,290:1 955-1 956.
[6] Xu X,Zhou ZH,Wang X L.The smallest known non-avian theropod dinosur[J].Nature,2000 ,408:705-708.
[7] Xu X,Zhou Z H,Prum R.Branched integumental structures in Sinomithsaurus and the origin of feathers [D].Nature,2001,410: 200-204.
[8] Zhou Zhiyan,Zheng Shaolin.The missing link in Ginkgo evolution[J].Nature ,2003 ,423:821-822.
[9] 季强辽西中生代热河生物群[M].北京:地质出版社,2004.
[10] 张立东,郭胜哲,张长捷,等.辽宁省四合屯-.上园地区珍稀化石沉积层的产出特征及其形成环境[D].中国地质,2001 ,28(6):10-20.
[11] 张招崇,李兆鼐,王富宝,等.辽西义县盆地火山岩的基本特征及其成因探讨[D].现代地质,1994,8(4):441-450.
[12] 郭胜哲,张立东,张长捷,等.辽宁西部义县组研究新进展[D].中国地质,2001,28(8):1-8.
[13] 高春玲,刘金远.辽宁北票发现-新的无尾两栖类[D].世界地质,2000,23(1):1-5.
[14] 董枝明,孙跃武,伍少远.辽西朝阳盆地早自垩世一新的无齿翼龙化石[J].世界地质,2003,22(1):1-7.
[15] 张宏,王五力,李之彤,等辽西北票和义县地区义县组综合对比研究[J].地质通报,2004,23(8):766-777.7.
[16] 刘金远,姬书安,唐烽,等辽西义县组恐龙类化石一新种[D].地质通报,2004,23(8):778-783.
[17] 孙革,郑书林,孙春林,等古果属Archae fruetws)研究进展及其时代的讨论[D].吉林大学学报(地球科学),2004,33(4):393.-398.
[18] 陈义贤,陈文寄.辽西及邻区中生代火山岩-年代学.地球化学和构造背景[M].北京:地展出版社,1997.
[19] 卢造勋,夏怀宽内蒙古东乌珠穆沁旗-辽宁东沟地学断面[D].地球物理学报,1993,36(6):765-772.
[20] 卢造勋,姜德录,白云,等中国东北地区深部地球物理探测与研究进展[A].见:张中杰,高锐,吕庆田,等.中国大陆地球深部结构与动力学研究一庆贺滕吉文院士从事地球物理研究50周年[C].北京:科学出版社,2004.475-482.
[21] 夏怀宽,卢造助,牛雪,等朝阳-义县地震区的深浅部构造。组成及其与地震的关系[D]地震学报,1992,14(2):180-186.
[22] 沃里沃夫斯基B C,萨尔基索夫IO M.世界最大的含油气盆地[M].任俞,译北京:石油工业出版社,1992.
[23] 顾芷娟.地壳低速高导层的物理性质[D].矿物岩石地球化学通报,2000,190):30-33.
[24] 顾芷娟.地壳内低速高导层成因初步探讨[D].中国科学(D辑),1995,25(1):108-112.
[25] 张景廉,朱炳泉,张平中,等地壳的新地球物理模型与石油的无机合成说[D].地球物理学进展,1997,12(4):91-97.
[26] 张景廉,于均民论中地壳及地质意义[D].新疆石油地质,2004,25(1):90-94.
[27] 张景廉论石油的无机成因[M].北京:石油工业出版社,2001.
[28] 李扬鉴,张星亮,陈延成大陆层控构造导论[M].北京:地质出版社,1996.
[29] 杜乐天.烃碱流体地球化学原理[M].北京:科学出版社,1996.
[30] 陈沪生.下扬子地区HQ-13线的综合地球物理调查及其地质意义[D].石油天然气地质,1988,9(3):211-222.
[31] 朱炳泉.地球化学省与地球化学急变带[M].北京:石油工业出版社,2001.
[32] 陈义贤,朱炳泉,张景廉,等.辽河断陷石油生成环境与演化[M].北京:石油工业出版社,999.100.
[33] 张景廉克拉2大气田成因讨论[D].新疆石油地质,2002,23(1):71-73.
[34] 谢学锦.化学定时炸弹研究[J].中国地质,1993,(11):18-19.
[35] 王登红,陈振宁,李建康中新生代以来地幔柱活动的全球响应[A].见:张中杰,高锐,吕庆田,等.中国大陆地球深部结构与动力学研究一庆贺滕吉文院士从事地球物理研究50周年[C].北京:科学出版社,2004.
[36] 甘克文.国内外油气勘探前景剖析[D].石油科技论坛,2004(5):21-25.
[37] 王铁冠,黄光辉,徐中一.辽西龙潭沟元古界下马岭组底砂岩古油藏探讨[J].石油与天然气地质,1988,9(3):278-286.
[38] 赵玉芬 ,赵国辉.元素有机化学[M].北京:清华大学出版社,1998.192-205.
[39] 袁润广.生命演化宏观形式溯源梗概[M].北京:地质出版社,2002.
[40] 股鸿福,黄思骥,张克信,等.华南二叠纪-三叠纪之交的火山活动及其对生物绝灭的影响[D].地质学报,1989,63.(4):285-294.
[41] Swisber I C s,WangYQ,Wang XL,et al.Cretaceous age for the feathered dinosaus of Liaon ing.China DJ].Nature,1999,400:58-61.
[42] 马宗晋,杜品仁,卢苗安.地球的多圈层相互作用[J].地学前缘,2001,8(1):3-8.
[43] 张景廉,朱炳泉.欧亚大陆大中型油气田分布规律探讨[J].新疆石油地质,2000,21(5):353-356.
[44] Zhu Bingquan,Zhang Jinglian,Tu Xianglin,et al Pb,Sr,Nd istopic features in organic matter from China and their implications for petroleum generation and migration [J].Geochimica et Cosmochimica Acta,2001,65(15):2555-2570.
[45] 张景廉,冯有奎,李相博.无机生油理论与21世纪中国油气勘探战略[D].新疆石油地质,2002,23(3):248-251.