1) Meso-Cenozoic
中、新生代
1.
The Meso-Cenozoic Tectonic Transitions in the Fuxin Basin, Liaoning and Their Geological Significances;
辽宁阜新盆地中、新生代构造转折及其地质意义
2.
Geological features and tectonic evolution of Meso-Cenozoic basins in southeastern China;
中国东南部中、新生代盆地特征与构造演化
3.
This paper focuses on the main basin prototypes developed in four tectonic evolution periods and their superposition in southern China during the Meso-Cenozoic.
本文主要论述了我国南方中、新生代四期构造变格发育的主要盆地原型及其在主要盆地的迭加特征,并根据中、新生代盆地原型的迭加方式和构造改造特点,将南方主要探区的海相中、古生界后期改造形式划分为五种类型,即:持续前渊*迭加型、渊-滑-断-拗迭加型、渊-滑/断迭加型、推覆构造及影子盆地型、残留改造型,进而分别探讨了它们的主要构造特点和在油气保存条件上的差异。
2) Mesozoic and Cenozoic
中、新生代
1.
Mesozoic and Cenozoic basin evolution and coal-derived gas accumulation of upper Paleozoic in the area of Bohai Bay Basin
中、新生代渤海湾盆地区演化与上古生界煤成气成藏
2.
Most of Mesozoic and Cenozoic bearing oil and gas basins are rifting ones in eastern China whose development closely is related with normal faults.
中国东部中、新生代含油气盆地众多 ,为断陷盆地类型 ,断层发育也往往表现为正断层形式。
3.
Based on the basin-range coupling theory,the tectonic geology events during Mesozoic and Cenozoic were determined from the point that East Kunlun orogenic belt and west-south Qadam basin were in a common stress field,combining with versatile data and filed geology review.
根据盆山耦合理论,从东昆仑造山带与柴西南盆地受制于共同应力场的角度,结合二者资料及野外考察,对东昆仑山中、新生代以来的构造事件进行了厘定。
3) Mesozoic-Cenozoic
中、新生代
1.
Mesozoic-Cenozoic five tectonic events and their petroleum geologic significances in west Tarim Basin;
塔里木盆地西部中、新生代5次构造事件及其石油地质学意义
2.
Formation and Disintegration of Mesozoic-Cenozoic Intra-Continental Ramp Zone in Middle and Lower Yangtze Region;
中、下扬子区中、新生代陆内对冲带的形成及解体
4) Mesozoic and Cenozoic time
中、新生代
1.
During the Mesozoic and Cenozoic time, the earth lithosphere experienced significant tectonic changes and finally shaped into the present-day feature of the Earth.
中、新生代是地球岩石圈经历重大构造演化 ,最终形成现今地球面貌的时代。
5) Mesozoic and Cenozoic Era
中、新生代
1.
Analysis of sedimentation and erosion of the Hefei basin has demonstrated that the basin experienced multi stage depression and uplifting in the Mesozoic and Cenozoic Era.
合肥盆地中、新生代经历了多次沉降和隆升变化，侏罗系沉积作用分布于整个盆地，中、晚侏罗世盆地内地层遭受广泛剥蚀。
6) Meso-Cenozoic
中新生代
1.
Analysis of joints from the Meso-Cenozoic tectonic stress field in the west section of south Dabashan fault-fold belt in China;
南大巴山褶断带西段中新生代构造应力场的节理研究
2.
Meso-Cenozoic tectonic setting and evolution of East China Sea shelf basin;
东海陆架盆地中新生代构造背景及演化
3.
Structural deformation mechanism of the Meso-Cenozoic basementand cover in the north Tarim uplift-Kuqa depression;
塔北隆起—库车坳陷区中新生代基底-盖层构造变形机理
补充资料：晚新生代大冰期
又称第四纪大冰期。晚新生代发生大规模冰川作用的时期。第三纪中期，全球气候开始转冷，自然地理带向中低纬度带及海拔低处推移，极地冰盖范围扩大，中低纬度的高山也发生冰川作用。除南极冰期始于第三纪中期外，其余地区多属第四纪冰期，距今24o万年前至距今1万年前。第四纪冰期的冰川规模很大，北半球大冰盖的南缘在欧洲抵达北纬50°左右，在北美大陆一直推进到北纬40°以南；南极洲的冰盖也比现今大得多。据估计，在晚更新世末次冰期的最盛时期，世界大陆有32％的面积被冰川覆盖，冰川总面积为现今的3倍，海平面下降130米左右，气温较今低3～7～11℃。第四纪大冰期的来临，对自然环境的演变及人类的进化部产生重大影响。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条