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辽宁西部义县组湖相枕状熔岩的发现及其意义
引用本文:张立东,郭胜哲,张长捷,彭艳东,贾斌,陈树旺,邢德和,丁秋红,郑月娟.辽宁西部义县组湖相枕状熔岩的发现及其意义[J].地球学报,2002,23(6):491-494.
作者姓名:张立东  郭胜哲  张长捷  彭艳东  贾斌  陈树旺  邢德和  丁秋红  郑月娟
作者单位:中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033; 东北大学,辽宁沈阳1100004;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033; 东北大学,辽宁沈阳1100004;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033; 东北大学,辽宁沈阳1100004;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033; 东北大学,辽宁沈阳1100004;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033; 东北大学,辽宁沈阳1100004;中国地质调查局沈阳地质矿产研究所,辽宁沈阳110033
基金项目:国土资源部区域地质调查项目“北票市等4幅1:5万地质填图”(编号:J4.1.12)
摘    要:通过详细的区调工作,在四合屯、三百垄等地发现了一系列源相枕状熔岩。研究表明,这些枕状熔岩产于同一地层层位--义县组二段,是珍稀化石沉积层中的火山岩夹层。它们除了代表一次灾变事件外,还反映出形成枕状熔岩的古湖泊接近最大湖泛期,并且水体较深。在这种环境下,生物快速繁衍。而强烈的火山作用使得大批生物死亡,形成了现今丰富的化石组合。这些枕状熔岩的发现对于准确确定珍稀动植物化石的形成时代和环境具有重要意义。

关 键 词:辽宁西部    义县组    枕状熔岩

The Discovery of Pillow Lavas in Yixian Formation, Western Liaoning, and Its Significance
ZHANG Li-dong,GUO Sheng-zhe,ZHANG Chang-jie,PENG Yan-dong,JIA Bin,CHEN Shu-wang,XING De-he,DING Qiu-hong and ZHENG Yue-juan.The Discovery of Pillow Lavas in Yixian Formation, Western Liaoning, and Its Significance[J].Acta Geoscientia Sinica,2002,23(6):491-494.
Authors:ZHANG Li-dong  GUO Sheng-zhe  ZHANG Chang-jie  PENG Yan-dong  JIA Bin  CHEN Shu-wang  XING De-he  DING Qiu-hong and ZHENG Yue-juan
Institution:Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004;Shenyang Institute of Geology and Mineral Resources, 110033; Northeast University, Shenyang, Liaoning, 110004
Abstract:A series of pillow lavas were discovered in such areas as Sihetun and Sanbailong through detailed geological survey. This paper describes characteristics of these pillow lavas. The lavas are intercalations in the sediments containing precious fossils, and occur in the same stratigraphic horizon-2nd Member of Yixian Formation. They represent a disastrous event and reflect the fact that the ancient lake where the pillow lavas were formed was then in the maximum expansion with rather deep water. In this environment, the living beings quickly increased and flourished, while the intense volcanism led to the death of many living things and the formation of abundant fossil assemblages. The discovery of pillow lavas is of great significance in precise determination of the forming age and living environment of the animals and plant fossils.
Keywords:western Liaoning  Yixian Fomation  pillow lava
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