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On the Carboniferous Sequence Stratigraphy in the Tazhong Area, Xinjiang——A Model of the Sequence Stratigraphy Framework of Intracratonic Depressional Basins 被引量:4
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作者 Guo Jianhua Zeng Yunfu Zhai Yonghong and Gao Zhenzhong Jianghan Petroleum Institute, Jingsha, Hubei Chengdu Institute of Technology, Chengdu, Sichuan Jianghan Petroleum Institute, Jingsha, Hubei Liu Xinzhu 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 1997年第3期328-343,共16页
The Carboniferous prototype sedimentary basin in the Tazhong (Central Tarimbasin) area is recognized as a compressive intracratonic depressional one. Three type Ⅰ sequenceboundaries and three type Ⅱ sequence boundar... The Carboniferous prototype sedimentary basin in the Tazhong (Central Tarimbasin) area is recognized as a compressive intracratonic depressional one. Three type Ⅰ sequenceboundaries and three type Ⅱ sequence boundaries can be identified in the CarboniferousSystem, which can accordingly be divided into five sedimentary sequences. These sequencespossess stratigraphic characters of the standard sequence and correspond to the depositionalstratigraphic unit of a third-order eustatic cycle. They can be regionally or globally correlatedwith each other. The framework of sequence stratigraphy of the intracratonict basin in thestudy area distinctly differs from that of the passive continental-margin basin in the lack ofdepositional systems of early-middle lowstand, poor development of the deeply incised valleyand condensed section of the maximum sea-flood, good development of type Ⅱ sequenceboundaries and coastal plain depositional systems coexisting with shelf-type fan deltas underwet climatic conditions, Which consequently led to the formation of a paralic lithofacies frame-work. 展开更多
关键词 sequence stratigraphy intracratonic depressional basin framwork model depositional system CARBONIFEROUS
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江陵浅水—半深水坳陷湖盆层序地层学特征 被引量:4
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作者 卢明国 林畅松 +1 位作者 廖忠礼 张建华 《沉积学报》 CAS CSCD 北大核心 2003年第2期313-317,共5页
以层序地层学理论为指导 ,系统研究了江陵浅水—半深水坳陷湖盆的层序地层学特征。研究表明 :区域不整合界面和沉积转换界面是 级层序的主要界面 ;层序内虽均发育低位、湖侵和高位体系域 ,但各体系域发育程度是不同的 ,致使层序的旋回... 以层序地层学理论为指导 ,系统研究了江陵浅水—半深水坳陷湖盆的层序地层学特征。研究表明 :区域不整合界面和沉积转换界面是 级层序的主要界面 ;层序内虽均发育低位、湖侵和高位体系域 ,但各体系域发育程度是不同的 ,致使层序的旋回性以非对称为主 ;层序内各体系域的沉积相构成均以河流三角洲和浅水湖泊为主 ,而冲积扇、扇三角洲不发育 ,湖泊水体基本没有发生过明显的扩张、收缩 ,湖平面的波动没有造成沉积相带的区域性变化 ,在此基础上 ,建立了江陵浅水—半深水坳陷湖盆特有的两种层序地层充填模式。 展开更多
关键词 沉积充填演化 层序地层 充填模式 江陵凹陷 沉积相 湖平面
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Different Kinetics of Puerarin in Plasma of Normal and Depressed Rats After Oral Administration of Chinese Medicine TZ18 被引量:11
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作者 申佳 孟甄 +3 位作者 苏慧 邢东明 丁怡 杜力军 《Tsinghua Science and Technology》 SCIE EI CAS 2007年第4期394-399,共6页
The objective of this study is to quantify the puerarin in rat plasma following oral administration of TZ18 and compare the pharmacokinetics characteristics of puerarin in normal rats with that in depression model rat... The objective of this study is to quantify the puerarin in rat plasma following oral administration of TZ18 and compare the pharmacokinetics characteristics of puerarin in normal rats with that in depression model rats. A high performance liquid chromatography method was used to quantify the puerarin due to its good selectivity and linearity (coefficient correlation, r^2 = 0.9991) within the tested range (0.028-0.889 μg·mL^-1)- Intra- and inter-day precision coefficients of variation and accuracy bias were acceptable (Maximum coefficient of variation was 5.74% for intra-day and 3.09% for inter-day) over the entire range. The recoveries were found to be 98.3%, 101.4%, and 103.4% for concentrations of 0.028, 0.222, and 0.444 μg · mL^-1, respectively. The concentration-time curves for both normal rats and depression model rats were fit to a twocompartment model with the first order absorption. The results show significant differences in the main pharmacokinetic parameters of peak time, peak concentration, and the area under the concentration-time curve between the two kinds of rats. 展开更多
关键词 PUERARIN depression rat model PHARMACOKINETICS
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