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- The Meso-Tethys was a sea lying between Laurasia and Gondwana during the Middle and Late Mesozoic. 中特提斯是中生代中晚期存在于南、北大陆之间的海洋。
- The main reservoir spaces in Archean are mainly tensional,steeply dipped fractures oriented in NE and NW directions and micro-cracks formed in the middle or the Late Mesozoic. 茨榆坨潜山储集空间主要是裂缝和微裂隙,太古界储层主要发育北东向和北西向两组裂缝,以高角度张性裂缝为主,形成于中生代中、晚期;
- The main reservoir spaces in Archean are mainly tensional, steeply dipped fractures oriented in NE and NW directions and micro-cracks formed in the middle or the Late Mesozoic. 茨榆坨潜山储集空间主要是裂缝和微裂隙，太古界储层主要发育北东向和北西向两组裂缝，以高角度张性裂缝为主，形成于中生代中、晚期；
- Young basic intrusives, which took place late Mesozoic times, formed numerous minor dolerite dykes. 这些早期的侵入性活动，发生在中生代早期，并形成了一些粗玄岩的沟壑。
- Tiefa basin is a late Mesozoic NNE-trending half graben coal-bearing basin,and the NWW structural system is the most important synbasinal structure. 铁法盆地属于晚中生代的NNE向半地堑煤盆地,北西西系是其主要的成盆期构造。
- There are many deep source xenoliths with different lithologic composition in late Mesozoic basalt of Huziyan, Daoxian County, Hunan Province. 湖南道县虎子岩玄武岩是中生代末期形成的,含有较多的岩性各异的深源岩石包体。
- Are the peridotitic xenoliths entrained in Late Mesozoic intermediatemafic intrusive complexes on the North China Craton the direct samples of lithospheric mantle? 华北晚中生代中基性侵入岩中橄榄岩捕虏体是岩石圈地幔直接样品?
- There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea. 南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
- The coastal area around Southeastern Fujian is located in the Changle-Nan'ao tectonic zone, where mafic dikes (swarms) were developed since late Mesozoic. 摘要闽东南沿海地处长乐-南澳构造带内，发育晚中生代以来的基性岩脉（岩群），其几何形态和产状记录着区域应力场活动。
- Title： Are the peridotitic xenoliths entrained in Late Mesozoic intermediate-mafic intrusive complexes on the North China Craton the direct samples of lithospheric mantle? 关键词：华北;晚中生代;中基性侵入岩;橄榄岩捕虏体;堆晶成因
- In the lowest part of the crust, mafic granulites which were resulted from fractional crystallization and cumulation of mantle-derived magma in Late Mesozoic are distributed. 在下地壳底部，分布著由晚中生代幔源岩浆分离结晶和堆晶的基性麻粒岩。
- Are the peridotitic xenoliths entrained in Late Mesozoic intermediate-mafic intrusive complexes on the North China Craton the direct samples of lithospheric mantle? 华北晚中生代中基性侵入岩中橄榄岩捕虏体是岩石圈地幔直接样品?
- Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic. 白音查干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。
- The coastal area around Southeastern Fujian is located in the Changle-Nan ao tectonic zone, where mafic dikes (swarms) were developed since late Mesozoic. 闽东南沿海地处长乐-南澳构造带内,发育晚中生代以来的基性岩脉(岩群),其几何形态和产状记录着区域应力场活动。
- According to the paleobiogeographic analysis,the Senjitu region belonged to temperate zone or warm climate condition and underwent four evolutionary episodes during late Mesozoic. 古地理分析表明森吉图地区在中生代晚期温暖的气候条件下共经历了4个演化阶段。
- Fuxin basin is a small sized rift subsidence basin of later Mesozoic in western Liaoning province. 阜新盆地是辽西地区的一个晚中生代小型断陷盆地，形成于晚侏罗世到早白垩世期间。
- In Late Mesozoic, the evolution of the Songliao basin progressed through 4 stages: thermal doming, rifting, depression and shrinkage. Corresponding to the late three stages: it developed three biotas, Jehol biota, Sungari biota and Mingsui biota. 松辽盆地晚中生代经历了热隆张、裂陷、坳陷和萎缩4 个地质演化阶段，后3 个阶段相应发育了三大生物群，即热河生物群、松花江生物群和明水生物群。
- Fuxin basin is a continental graben basin of the Mesozoic. Based on the strata of the Archean and the mid-Proterozoic it was filled with two coal-bearing series of rocks during the late Mesozoic,named Shahai Group and Fuxin Group. 阜新盆地是中生代陆相断陷型盆地,由太古界、中元古界组成盆地基底,其上接受了晚中生代地层沉积,包括沙海组、阜新组两套含煤岩系。
- Besides, the two important problems, the deep prooes of lithosphere and the inversion of tectonic stress field, have to be expounded for studying the geodynamic setting of the Late Mesozoic rifting. 此外．对晚中生代裂陷作用的动力学背景的探讨需要阐明岩石圈的深部过程和构造应力场的反转这个两个重要的问题。
- I'm sick of being piggy in the middle all the time. 我腻烦了总是夹在争吵双方的中间。
