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21篇 您的检索式:作者名="Pubellier"
    题名 作者 年代 出处 被引量
1跨南海西南次海盆OBS、多道地震与重力联合调查显示文摘对跨南海西南次海盆及两侧陆缘的一条1050km长的、包括海底地震(OBS)、长排列多道地震和重磁在内的综合地球物理探测剖面(CFT)进行了构造成像和研究。在多道地震成像基础上建立了CFT剖面初始速度模型,进而通过初至波层析成像方法反演了CFT剖面的速度结构模型,在重力异常资料的约束下建立了CFT剖面的综合地壳结构模型。讨论了沿CFT剖面出现的下地壳高速体、龙门海山的低密度物质等地质问题。结果表明,下地壳高速层在北部陆坡、西南海盆和南部南沙地块均有分布,厚度在0~4km之间,可能与陆缘下地壳物质和地幔物质熔融混合,以及深海盆海底扩张期间构造拉伸导致地幔蛇纹岩化有关。汪俊 邱燕 阎贫 DELESCLUSE M 王彦林 PUBELLIER M 聂鑫 2019热带海洋学报2019,38,4:7
2南海西南次海盆构造特征及其沉积响应显示文摘本文对穿过南海西南次海盆的逾1000 km的多道地震测线CFT剖面进行了地震界面特征的识别和地震层序的划分,分段分析了拆离断层对其减薄陆壳的拆离作用。结合前人研究成果,对南海西南次海盆地壳结构特征开展了分析,并总结了其构造特征。西南次海盆在发生陆缘张裂—海盆扩张、洋壳出现—扩张后稳定沉积这一系列过程中,可划分为4个阶段的沉积响应:A阶段(古新世之前)——前裂谷阶段,表现为地壳在拉张应力下产生小的断层;B阶段(始新世—早渐新世)——陆缘的裂谷阶段,地壳在拉张应力下拉张减薄,A阶段产生的断层出现了旋转,出现了大型掀斜的拆离断层,沉积物为同裂谷沉积,该阶段以产生了破裂不整合结束;C阶段(晚渐新世—早中新世)——海盆扩张阶段,海盆开始扩张,张应力从陆缘转移到了洋盆;D阶段(中中新世以来)——海盆扩张结束以后,以一套稳定沉积为特征。聂鑫 邱燕 Manuel Pubellier 汪俊 朱荣伟 杜文波 2020中国地质2020,47,5:2
3Structural Restoration of Carbonate Platform in the Southern Part of Central Luconia, Malaysia显示文摘Carbonates of Central Luconia, Malaysia, had been serving as hydrocarbon reservoirs for more than 25 years. However, the relationship and impacts of extensive tectonic events to the growth of Miocene carbonates in Central Luconia have not been revealed sufficiently. In this work, two carbonates platforms in the southern part of Central Luconia were used for detailed interpretation and seismic based structural restoration. This work had provided new insight for the interpretation of carbonate growth in Central Luconia and its association with the surrounding tectonic. This work suggested three possible tectonic evolutions from Late Oligocene to Pliocene are responsible for the growth of carbonates in Central Luconia. These stages are equivalent with pre-carbonate stage(Late Oligocene–Early Miocene), syn-carbonate stage(Middle–Late Miocene) and post-carbonate stage(Pliocene). Rifting of the South China Sea and subduction of proto-South China Sea are believed to be responsible for the development of faulting during pre-carbonate stage, while movement of the ancient Baram Line is thought to control the parallel striking direction of normal faults during syncarbonate stage. Finally, subsidence and compaction due to the overburden clastic materials from the prograding deltas is considered as the main reason for the impacts of gravitational tectonics in this area, which corresponding to the post-carbonate stage.Siti Nur Fathiyah Jamaludin Manuel Pubellier David Menier 2018Journal of Earth Science2018,29,1:2
4Plate kinematics, origin and tectonic emplacement of supra-subduction ophiolites in SE Asia显示文摘Pubellier M Morley C Maury R 2004Tectonophysics2004,392,1:1
5Magmatic source enrichment by slab-derived melts in a young post-collisional setting, central Mindanao (Philippines) 显示文摘Sajona F G Maury R C Pubellier M 2000Lithos2000,54,:1
6Magmatic source enrichment by slab-derived melts in a young post-colli-sion setting,central Mindanao(Philippines)显示文摘Sajona F G Maury R C Pubellier M 2000Lithos2000,54,:1
7Polyphase rifting of greater Pearl River Della region ( South China ) : Evidence for possible rapid changes in regional stress configuralion显示文摘CHAN L S SHEN W PUBELLIER M 2010Journal of Structural Geology2010,32,74:1
8Magmatic response to abrupt changes in geodynamic settings:Pliocene-Quaternary calc-alkaline and Nb-enriched Lavas from Mindanao (Philippines)显示文摘Sajona F G Bellon H Maury R C Pubellier M Cotten J Rangin C 1994Tectonophysics1994,237,12:1
9A simple model for the tectonic evolution of southeast Asia and Indonesia region for the past 43 Ma 显示文摘Rangin C Jolivet L Pubellier M 1990Bulletin de la Societe geologique de France1990,8,6:1
10Cenozoic deformation in western Yunnan(China- Myanmar border) 显示文摘SocquetA Pubellier M 2005Journal of Asian Earth Sciences2005,24,:1
11A simple model for the tectonic evolution of southeast Asia and Indonesia region for the past 43 Ma显示文摘RANGIN C JOLIVET L PUBELLIER M 1990Bulletin de la Societe Geologique de France1990,8,6:1
12Tomographic and geological constraints on subduction along the eastern Sundaland continental margin (SouthEast Asia) 显示文摘Rangin C Spakman W Pubellier M 1999Bull SOc Geol Fr1999,170,:1
13Cenozoic deformation in western Yunnan(China-Myanmar border)显示文摘Socquet A Pubellier M 2005Journal of Asian Earth Sciences2005,24,:1
14Initiation of subduction and the generation of slab melts in western and eastern Mindanao, Philippines显示文摘Sajona FC Maury RC Bellon H Cotten J Defant M J Pubellie M Rangin C 1993Geology1993,21,:1
15Cenozoic Deformation in Western Yunnan(China-Myanmar Border)显示文摘Anne Socquet Manuel Pubellier 0,,:1
16Tomographic and geological constraints on subduction along the eastern Sundaland continental margin (South-East Asia)显示文摘Rangin C Spakman W Pubellier M 0,,:1
17The final rifting evo lution in the South China Sea显示文摘Franke D Savva D Pubellier M el al 2013Marine and Petroleum Ge- ology2013,,:1
18Seismic evidence of hype>stretched crust and mantle exhumation offshore Viet nam显示文摘Savva D Meresse F Pubellier M 2013Tectonophysics2013,608,:1
19Tomographic and geological constraints on subduction along the eastern Sundaland continental margin (South-East Asia) 显示文摘Rangin C Spakman W Pubellier M 1999Bul- letin de Ia Societe Geologique de France1999,170,6:1
20Initiation of subduction and the generation of slab melts in western and eastern Mindanao, Philippines 显示文摘Sajona F G Maury R C Bellon H Cotton J Defant M J Pubellier M 1993Geology1993,21,11:1
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