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辽东北—吉南中生代火山岩地层与辽西义县组的对比 被引量:9
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作者 陈井胜 李斌 +5 位作者 姚玉来 刘淼 杨帆 邢德和 李伟 汪岩 《地质学报》 EI CAS CSCD 北大核心 2016年第10期2733-2746,共14页
辽宁东北部桓仁—吉林南部通化地区分布有大面积的中生代火山岩,分别属于果松组、林子头组及小岭组。通过野外地质调查发现,这三个组的火山岩组合自下而上均显示为酸性—中性—酸性的岩石组合,在岩石组合上具有可对比性。对这三个组的... 辽宁东北部桓仁—吉林南部通化地区分布有大面积的中生代火山岩,分别属于果松组、林子头组及小岭组。通过野外地质调查发现,这三个组的火山岩组合自下而上均显示为酸性—中性—酸性的岩石组合,在岩石组合上具有可对比性。对这三个组的典型火山岩进行LA-ICP-MS锆石U-Pb测年,结果显示果松组安山岩(GS-1-TWS)和流纹岩(GS-2-TWS)年龄为130.83±0.8Ma和118.5±1.1Ma;林子头组安山质凝灰岩(LZT1)和安山岩(LZT2)年龄为123.24±0.91Ma和126.0±2.9Ma;小岭组流纹岩(P03-29)和安山岩(P03-30)年龄为126.3±1.3Ma和129.0±1.4Ma,表明三个含有中生代火山岩的地层形成时代一致,均为早白垩世产物。辽西地区含有中生代火山岩的地层为义县组,其形成时代为133-118Ma之间,本文辽宁桓仁—吉林通化地区中生代火山岩形成时代为130-118Ma,二者为同时产物;并且二者均产有相同的热河生物群化石,所以辽东北—吉南果松组、林子头组、小岭组与辽西义县组可对比。! 展开更多
关键词 辽东北—吉南 中生代火山岩地层 果松、林子头及小岭 LA-ICP-MS锆石U-Pb 辽西义县组
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辽西鸟类化石层沉积时期的气候环境
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作者 朱为庆 《化石》 2000年第2期27-28,共2页
关键词 辽西北景义县 鸟类化石层 气候环境 潮湿环境
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Palynomorph assemblages and paleoclimate records from the Zhuanchengzi Bed of the Yixian Formation, western Liaoning Province, China 被引量:5
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作者 CUI Ying GONG EnPu +3 位作者 WANG TieHui GUAN ChangQing ZHANG YongLi LIANG JunHong 《Science China Earth Sciences》 SCIE EI CAS CSCD 2015年第9期1538-1552,共15页
We collected, processed, identified, and analyzed the spores and pollen samples from the Zhuanchengzi Bed of the Yixian Formation in the Yingwoshan area of western Liaoning. As a result, we confirm a palynomorph assem... We collected, processed, identified, and analyzed the spores and pollen samples from the Zhuanchengzi Bed of the Yixian Formation in the Yingwoshan area of western Liaoning. As a result, we confirm a palynomorph assemblage of Cicatri- cosisporites-Protoconiferus. The pollen was primarily from gymnosperms, dominated especially by conifer pollen. Pterido- phyte spores were less common and some questionable angiosperm pollen occurred occasionally. The age of the palynomorph assemblage is dated as the late Valanginian or Hauterivian-Barrernian stage, the Early Cretaceous. The study applies the con- cept of Palynological Vegetation based on palynological spectra and the paleoecological characteristics of palynological taxa for the first time. Palynological vegetation type, climatic zone type, and humidity type are divided quantitatively for the Zhuanchengzi Bed in the Yixian Formation of western Liaoning. We then obtained the evolutionary trends. The results showed that the overall climate was warm and humid during the deposition period of the Zhuanchengzi Bed in the Yixian Formation. Palynological vegetation types are various and include coniferous forest, deciduous broadleaf forest, evergreen broad-leaved forest, grass, and shrubs. The local temperature changed from warm to much warmer and from a semi-humid to humid climate. Palynological vegetation types are always dominated by coniferous forest. The coexistence of deciduous broad-leaved forest, evergreen broad-leaved forest, shrubs, grass, and some xerophytic plants indicates vertical zonation and seasonal climate change The vertical vegetation types and the warm humid climate may imply a large geomorphological contrast in the Yixian Formation of western Liaoning. 展开更多
关键词 palynomorph assemblage PALEOCLIMATE vertical zonation of vegetation Zhuanchengzi Bed Yixian Formation
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