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南海共轭大陆边缘构造属性的综合地球物理研究 被引量:55
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作者 郝天珧 徐亚 +6 位作者 孙福利 游庆瑜 吕川川 黄松 丘学林 胡卫剑 赵明辉 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2011年第12期3098-3116,共19页
利用南海最新的重磁资料,在岩石物性分析和全海域分带变倾角化极磁异常反演磁性基底分布的基础上,选择6条典型剖面拟合反演其密度与磁性结构,在此基础上进行了深部结构的对比分析.反演中尽可能以海底地震仪探测数据(OBS)、多道地震等结... 利用南海最新的重磁资料,在岩石物性分析和全海域分带变倾角化极磁异常反演磁性基底分布的基础上,选择6条典型剖面拟合反演其密度与磁性结构,在此基础上进行了深部结构的对比分析.反演中尽可能以海底地震仪探测数据(OBS)、多道地震等结果作为约束,其中FF'剖面层速度分析是利用"南海大陆边缘动力学及油气资源潜力"973项目2009年最新采集的多道地震数据,并利用了OBS2009南沙段数据对重力数据进行了物性结构拟合反演.根据剖面深部结构与物性分布特征分析认为:南海北部、南部陆缘均应以非火山型构造属性为主.北部陆缘CC'剖面以东,虽有下地壳高密度层存在并伴有活跃的岩浆活动,但缺乏典型向海倾斜反射层(SeawardDipping Reflectors)存在的证据,推断高密度层应与浅表岩浆岩一样,是海底扩张之后陆缘裂解过程中的产物.中沙隆起与礼乐盆地区的磁性基底和深部结构特征十分相似,推断在海盆拉张之前应为同一块体,属于共轭大陆边缘中的"共轭点".西南次海盆南部陆缘地球物理综合分析表明:在陆坡坡脚附近有中生界分布,但层速度计算结果表明可能整条剖面上的中生界并不完全连续. 展开更多
关键词 南海 共轭大陆边缘 物性拟合剖面 构造属性 综合地球物理解释
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Image Analysis of Fabric Pilling Based on Light Projection 被引量:3
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作者 陈霞 黄秀宝 《Journal of Donghua University(English Edition)》 EI CAS 2003年第4期1-4,共4页
The objective assessment of fabric pilling based on light projection and image analysis has been exploited recently.The device for capturing the cross-sectional images of the pilled fabrics with light projection is el... The objective assessment of fabric pilling based on light projection and image analysis has been exploited recently.The device for capturing the cross-sectional images of the pilled fabrics with light projection is elaborated.The detection of the profile line and integration of the sequential cross-sectional pilled image are discussed.The threshold based on Gaussian model is recommended for pill segmentation.The results show that the installed system is capable of eliminating the interference with pill information from the fabric color and pattern. 展开更多
关键词 fabric pilling image analysis of fabric pilling light projection image edge detection of projected profile pill segmentation
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Edge Plasma Profiles Measured by Fast Reciprocating Probes System on HL-2A Tokamak
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作者 CHENG Jun YAN Longwen HONG Wenyu QIAN Jun 《Southwestern Institute of Physics Annual Report》 2005年第1期25-27,共3页
Fast reciprocating probe systems ( FRPS ) are widely used in some tokamaks, such as JT- 60 U, TEXT and DIlI-D. The parameters with high temporal-spatial resolution are measured for boundary plasmas using these syste... Fast reciprocating probe systems ( FRPS ) are widely used in some tokamaks, such as JT- 60 U, TEXT and DIlI-D. The parameters with high temporal-spatial resolution are measured for boundary plasmas using these systems. The FRPS on HL-2A is developed, which is composed of transmission bar, digital grating displacement system, electromagnetic valves, stepping motor and so on. The high-pressure gas from the electromagnetic valves controlled by trigger signals provides the power to drive the transmission bar forward or backward. Reciprocating distance is 8 cm with the maximum speed of 1.5 m·s^-1. 展开更多
关键词 Fast reciprocating probe system Edge profiles
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Sedimentary features of the Permian-Triassic boundary sequence of the Meishan section in Changxing County,Zhejiang Province 被引量:4
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作者 ZHENG QuanFeng CAO ChangQun ZHANG MingYuan 《Science China Earth Sciences》 SCIE EI CAS 2013年第6期956-969,共14页
The Global Stratotype Section and Point(GSSP) for the Permian-Triassic boundary was placed in Bed 27 of Meishan section D where the conodont species Hindeodus parvus first occurs.Bed 27 was usually considered comprisi... The Global Stratotype Section and Point(GSSP) for the Permian-Triassic boundary was placed in Bed 27 of Meishan section D where the conodont species Hindeodus parvus first occurs.Bed 27 was usually considered comprising continuouslydeposited,homogeneous silty limestone,with no depositional hiatus near the boundary.Detailed study on the boundary sequence revealed that a typical firmground characterized by Glossifungites ichnofacies developed about 2 cm below the Permian-Triassic boundary in Bed 27.Fossil content and lithology show apparent differences across the firmground crust.The abundance of the Permian bioclasts decreases significantly across the firmground,and is accompanied by a shift of dominating carbonate precipitation from calcite to dolomite.The firmground marked a rapid transgression at the very end of the Late Permian and significant shifts of sedimentary environment and paleoclimate.This transgressive submerging surface is also observed at the Huangzhishan section of the shallow-water carbonate platform facies in Zhejiang Province,the Jiangya section of the lower-slope to basinal-margin facies in Hunan Province,the Pingdingshan section of the basinal facies in Anhui Province of South China,as well as the Selong section in Tibet of the northern peri-Gondwana.The transgressive submerging surface marks the onset of a rapid global transgression at the latest Permian. 展开更多
关键词 Meishan section Permian-Triassic boundary sedimentary features transgressive submerging surface
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