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| 黑龙江汤原断陷第三纪地层层序及时代 | |
| 引用本文： | 杨建国,黄清华,吴朝东,吴河勇.黑龙江汤原断陷第三纪地层层序及时代[J].地层学杂志,2004,28(2):168-172,184. |
| 作者姓名： | 杨建国 黄清华 吴朝东 吴河勇 |
| 作者单位： | 1. 北京大学,北京,100871;大庆油田有限责任公司勘探开发研究院,黑龙江,大庆,163712 2. 中国地质大学,北京,100083;大庆油田有限责任公司勘探开发研究院,黑龙江,大庆,163712 3. 北京大学,北京,100871 4. 大庆油田有限责任公司勘探开发研究院,黑龙江,大庆,163712 |
| 基金项目： | 大庆油田有限责任公司资助项目 |
| 摘 要： | 依据黑龙江汤原断陷30口井的岩性及古生物资料,建立了汤原断陷古近纪、新近纪地层层序。依据孢粉、藻类、植物和介形类化石建立19个生物化石组合,讨论了各组的时代及其与邻区的对比。依据汤参3井(25.0-100.0m)和互6井(138.5-237.5m)岩性及孢粉组合将道台桥组引入汤原断陷。汤原断陷地层层序为古新统乌云组,始新统新安村组、达连河组,渐新统宝泉岭组,中新统富锦组,上新统道台桥组。 |
| 关 键 词： | 汤原断陷 黑龙江 古近纪 新近纪 地层层序 时代 |
| 文章编号： | 0253-4959(2004)02-0168-05 |
SEQUENCES AND AGES OF THE PALEOGENE AND NEOGENE STRATA IN THE TANGYUAN RIFT,HEILONGJIANG |
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| YANG Jian-guo,HUANG Qing-hua,WU Chao-dong,WU He-yong Peiking University,Beijing, Geoscience University of China,Beijing, Exploration and Development Research Institute of Daqing Oilfield Co. Ltd.,Daqing.SEQUENCES AND AGES OF THE PALEOGENE AND NEOGENE STRATA IN THE TANGYUAN RIFT,HEILONGJIANG[J].Journal of Stratigraphy,2004,28(2):168-172,184. | |
| Authors: | YANG Jian-guo HUANG Qing-hua WU Chao-dong WU He-yong Peiking University Beijing Geoscience University of China Beijing Exploration and Development Research Institute of Daqing Oilfield Co Ltd Daqing |
| Institution: | YANG Jian-guo,HUANG Qing-hua,WU Chao-dong,WU He-yong Peiking University,Beijing,100871 Geoscience University of China,Beijing,100083 Exploration and Development Research Institute of Daqing Oilfield Co. Ltd.,Daqing,163712 |
| Abstract: | The Paleogene and Neogene strata in the Tangyuan Rift have been collated on the basis of litho- logic characters and fossils of 30 drilling-wells. 19 fossil assemblages have been established on the basis of fossil sporo-pollen, plants, algae, megaspore and ostracodes. The age of each formation in the Rift is dis- cussed and the strata in the Tangyuan Rift wi1l be correlated with the strata of the neighboring regions. Ac- cording to lithologic characters and sporo-pollen assemblages of Tangcan 3 well (25.0-100. 0m) and Hu 6 well (138.5-237.5m),the Daotaiqiao Formation is used in the Tangyuan Rift. Therefore the sequences of Paleogene strata in the Tangyuan Rift are respectively the Paleocene Wuyun Formation, Eocene Xinanchun and Dalianhe Formations, and Oligocene Baoquanling Formation. the sequence of Neogene strata in the Tangyuan Rift are respectively the Miocene Fujin Formation and Pliocene Daotaiqiao Formation. |
| Keywords: | Tangyuan Rift Heilongjiang Paleogene Neogene stratigraphic sequence age |
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