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宝月组
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     Group B: SD to Wistar rat heart tarnsplantation;
     B
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     Group E is the highest.
     B
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     ORIGIN OF DRY GASES IN BAOYUE DISTRICT, SANSHUI BASIN
     三水盆地宝月地区干气的成因探讨
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     Finally, according to the matching relation among source-reservoir-caprock during sedimentary evolutionary process, it was pointed out that Baoyue area in the western of the basin is the most favorable place for oil and gas exploration, and the Buxin Formation in the Paleogene is the beat layer, where the most favorable sedimentary system was developed on Dagang Member, including alluvial fan, fan-delta and delta.
     最后,根据沉积演化过程中的生储盖匹配关系,指出盆地西部宝月地区为最有利的油气勘探区块,最有利的层位为古近系怖心组,最有利的沉积体系为发育在怖心组大岗段之上的冲积扇、扇三角洲和三角洲。
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Paleomagnetic study of Sanshui Basin in Guangdong from Upper Cretaceous to Eocene Sanshui Formation (F.), Dalangshan F., Xingzhuang E., Buxing F., and Baoyue F., authors draw following conclusions: (1) Rotation movements were the main form of tectonic movements, corresponding to Basin's rifting and growing when clockwise (CW) rotation occurred and dying away when counterclockwise (CCW) rotation occurred, the extend of Basin's growth depended on the angles of rotation 1 (2) The turn of rotation direction from...

Paleomagnetic study of Sanshui Basin in Guangdong from Upper Cretaceous to Eocene Sanshui Formation (F.), Dalangshan F., Xingzhuang E., Buxing F., and Baoyue F., authors draw following conclusions: (1) Rotation movements were the main form of tectonic movements, corresponding to Basin's rifting and growing when clockwise (CW) rotation occurred and dying away when counterclockwise (CCW) rotation occurred, the extend of Basin's growth depended on the angles of rotation 1 (2) The turn of rotation direction from CW to CCW in Eocene fairly fitted with the action direction's change of Pacific-Kula Plate to Eurasia, indicates that Sanshui Basin was perhaps caused by the action of Pacific-Kula to Eurasia ; (3) The South China Block, in which Sanshui Basin is located, underwent no large latitudinal movements from Late Cretaceous to Eocene, but remained in a lower latitude position than the present's.

对广东三水盆地上白垩统三水组、大 山组、古新统莘庄组及始新统 心组、宝月组的系统的古地磁研究结果表明:(1)旋转运动是该区构造运动的主要形式,顺时针旋转盆地拉张发育,这时针旋转盆地挤压衰亡,发育的程度与旋转角度有关;(2)始新世该区旋转方向由顺时针旋转变为道时针旋转,对应于太平洋-库拉板块对欧亚板块作用方向的改变,说明三水盆地的形成发育与太平洋-库拉板块对欧亚板块的作用密切相关;(3)三水盆地所在的华南地块从晚白垩世至始新世在纬向上不存在明显的运动,一直停留在略低于现今纬度的位置上。

Multiple stratigraphical classification and correlation are carried out in Lubao-Datang area,Sanshui,Guangdong Province,and the Eogene strata are divided into the Xinzhuangcun Fm.,Buxin Fm.,Baoyun Fm.and Huayong Fm..Various fossils including charophyta,ostracoda,gasteropod,bivalve,fish and plant of more than 60 species and 25 genera have been found for the first time in the study area, which can be assorted to 7 fossil assemblages.Correlation of lithostratigraphical sequence and fossil assemblages shows that...

Multiple stratigraphical classification and correlation are carried out in Lubao-Datang area,Sanshui,Guangdong Province,and the Eogene strata are divided into the Xinzhuangcun Fm.,Buxin Fm.,Baoyun Fm.and Huayong Fm..Various fossils including charophyta,ostracoda,gasteropod,bivalve,fish and plant of more than 60 species and 25 genera have been found for the first time in the study area, which can be assorted to 7 fossil assemblages.Correlation of lithostratigraphical sequence and fossil assemblages shows that the biota was formed in continental facies fresh water environment during Paleocene-Eocene period in the condition of hot and arid climate.Himalayan orogeny made the area uplift to continent,confirming that the late-Paleocene coast line was probably at southeast Nanbianzhen-Shuiguowei-Jitang area.

对研究区内地层进行了多重划分对比,将古近纪地层划分为莘庄村组、土布心组、宝月组和华涌组4个岩石地层单位,并在该地层中首次发现轮藻、介形虫、腹足类、双壳类、鱼类、植物6个门类7个化石组合25属60余种生物化石,填补了本区生物地层的空白。根据岩石地层层序、生物组合特征和7个动植物化石组合的国内外对比,确定其形成时代为古新世-始新世,形成环境为陆相淡水,气候干旱、炎热。喜马拉雅运动使本区抬升为陆地,进一步证实晚古新世海侵边界大致在南边镇-水锅尾-基塘连线之南东地带。

 
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