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REDUCED AUGMENTED LAGRANGIAN BI-CONJUGATE GRADIENT METHOD FOR IMPACT-CONTACT PROBLEMS

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Acta Mechanica Solida Sinica 1998年第3期11卷 241-252页

作者： Li nansheng sha Desong Sun Huanchun Dalian Univ Technol Dept Engn Mech Dalian 116023 Peoples R China

To avoid the numerical oscillation of the penalty method andnon-compatibility with ex- plicit operators of conventional Lagrangemultiplier methods used in transient contact problems to en- forcesurface contact conditions, a new approach to enforcing surfacecontact constraints for the tran- sient nonlinear finite elementproblems, referred to as 'the reduced augmented Lagrangianbi-conjugate gradient method (ALCG)', is developed in this *** on the nonlinear constrained optimization theory and iscompatible with the explicit time integration scheme, this approachcan also be used in implicit scheme naturally.

关键词： impact-contact problems contact constraints explicit scheme

New record of the feather star Palaeocomatella hiwia(Echinodermata:Crinoidea:Comatulida)from Zhenbei Seamount in South China Sea:new insights into the taxonomic position of Palaeocomatella

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Journal of Oceanology and Limnology 2024年第1期42卷 244-251页

作者： shao’e SUN Zijie MEI Zhongli sha Jing WANG nansheng CHEN Department of Marine Organism Taxonomy and Phylogeny Institute of OceanologyChinese Academy of SciencesQingdao 266071China CAS Key Laboratory of Marine Ecology and Environmental Sciences Institute of OceanologyChinese Academy of SciencesQingdao 266071China Laoshan Laboratory Qingdao 266237China shandong Province Key Laboratory of Experimental Marine Biology Institute of OceanologyChinese Academy of SciencesQingdao 266071China Center for Ocean Mega-Science Chinese Academy of SciencesQingdao 266071China University of Chinese Academy of Sciences Beijing 100049China

One specimen belonging to the family Comatellinae was collected from the Zhenbei Seamount(332.5–478.2 m)in the South China Sea in July *** on the morphological characters,the specimen was identified as Palaeocomatella hiwia McKnight,*** is first recorded from China Sea and redescribed in *** specimen differs from the original description from New Zealand for never showing syzygy at br4+5 or br5+6 on interior and br1+2 on exterior ***,it is much conform to the redescription to specimens from Indonesia,with only differences in position of the second syzygy and distalmost pinnule *** is deposited in the Institute of Oceanology,Chinese Academy of *** analyses based on the mitochondrial c oxidase subunit I(COI)and 16S rRNA genes indicated that *** was nested within the tribe Phanogeniini and clustered with Aphanocomaster ***,*** showed same morphological features in terms of mouth placement,comb location,and number of comb teeth rows as other genera of ***,we suggest that the genus Palaeocomatella should be put in the tribe Phanogeniini.

关键词： new record Palaeocomatella hiwia McKnight 1977 South China Sea phylogenetic relationship taxonomy

渤海湾盆地辽河坳陷西部冷家——雷家地区中-深层超压成因及其对油气成藏的影响

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石油与天然气地质 2024年第1期45卷 130-141页

作者：陈昌邱楠生高荣锦周晓龙孙永河杨琳琳付健中国石油大学(北京)地球科学学院北京102249 中国石油辽河油田公司勘探开发研究院辽宁盘锦124010 重庆科技大学石油与天然气工程学院重庆401331 东北石油大学地球科学学院黑龙江大庆163318

为了研究渤海湾盆地辽河坳陷西部冷家—雷家地区中-深层超压发育形成机制及油气运移和成藏对该地区中-深层油气勘探的意义,基于实测地层压力和温度数据、测井数据及构造分析,对冷家—雷家地区中-深层超压发育特征、成因机制及超压在成... 详细信息

为了研究渤海湾盆地辽河坳陷西部冷家—雷家地区中-深层超压发育形成机制及油气运移和成藏对该地区中-深层油气勘探的意义,基于实测地层压力和温度数据、测井数据及构造分析,对冷家—雷家地区中-深层超压发育特征、成因机制及超压在成藏过程中的作用进行了综合分析。研究表明:(1)冷家—雷家地区发育超压型、常压型和低压型3类地层温度-压力系统,其超压段主要集中在洼陷带的沙河街组三段(沙三段)和沙河街组四段(沙四段),深度约为2 500~4 000 m;(2)超压形成机制以欠压实作用为主,伴有生烃增压、成岩作用和构造挤压作用贡献;(3)冷家—雷家地区主要存在超压带内部的油气自生自储型运聚和油气从超压带向常压/低压带的跨压力系统运聚2种运聚模式,前者主要发生在洼陷带内的沙三段和沙四段超压带内部,后者则为断裂活动期陈家洼陷沙四段烃源岩中的油气在超压驱动下向雷家和高升构造带充注,及冷家地区沙三段下亚段-沙三段中亚段超压带中的油气通过砂体和断裂输导向东部陡坡带和兴隆台潜山运聚。

关键词：超压成因机制成藏模式中-深层冷家—雷家地区辽河坳陷

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渤海海域现今地温场分布特征

石油与天然气地质 2009年第4期30卷 412-419页

作者：邱楠生魏刚李翠翠张媛郭永华中国石油大学油气资源与探测国家重点实验室北京102249 中国石油大学盆地与油藏研究中心北京102249 中海石油(中国)有限公司天津分公司技术部天津300452

渤海海域平均大地热流值为(60.9±8.7)mW/m2,其中石臼坨凸起、沙磊田凸起和渤南凸起热流值高达70～80mW/m2,渤中凹陷、黄河口凹陷和秦南凸起次之,其热流值也达到65～75mW/m2,辽东湾、庙西、莱州湾、歧口、沙南、埕北等地区热流值较低,... 详细信息

渤海海域平均大地热流值为(60.9±8.7)mW/m2,其中石臼坨凸起、沙磊田凸起和渤南凸起热流值高达70～80mW/m2,渤中凹陷、黄河口凹陷和秦南凸起次之,其热流值也达到65～75mW/m2,辽东湾、庙西、莱州湾、歧口、沙南、埕北等地区热流值较低,基本上都在65mW/m2以下。渤海海域平均地温梯度为30.8℃/km,但各构造单元存在差异,其中沙磊田凸起、渤中、渤南、石臼坨等地区地温梯度明显较高,一般为32～42℃/km之间;凹陷区地温梯度低,一般为22～32℃/km之间。渤海海域地温场的分布与渤海海域的构造形态相似,大体反映了北北东走向的郯庐断裂构造型态。

关键词：大地热流地温梯度地温场渤海海域