1) Meso-Cenozoic
中-新生代
1.
This dissertation is composed of the study on fission track method and application fission track method, combined with 40Ar/39Ar(K-Ar) method to study the Indosinian tectonic events and Meso-Cenozoic uplifting and exhumation of the Yunkaidashan.
本论文分两部分,第一部分是裂变径迹方法研究,第二部分是应用裂变径迹方法,结合~40Ar/~39Ar(K-Ar)法研究云开大山印支构造事件与中-新生代的隆升剥露作用。
2.
It is also a complicated Meso-Cenozoic petroliferous basin.
地理上属于泰勒-阿特拉斯的一部分,濒临地中海,是一个复杂的中-新生代海相叠合含油气盆地。
2) Mesozoic-Cenozoic
中-新生代
1.
Characteristics and formation mechanism of the faults in Mesozoic-Cenozoic in Jiyang Depression;
济阳坳陷中-新生代断裂发育特征及形成机制
2.
Geochemical Characteristics of Major Elements of Mesozoic-Cenozoic Basaltic Rocks from Eastern China;
中国东部中-新生代玄武质火山岩的主量元素地球化学特征
3.
The Mesozoic-Cenozoic Superposing Basin of Jiyang Depression and Oil-Gas Accumulation
济阳坳陷中-新生代叠合盆地及油气成藏
3) 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
4) Mesozoic-Cenozoic
中新生代
1.
Discussion on Mesozoic-Cenozoic Evolution of Tian Shan and Its Adjacent Basins;
中新生代天山及其两侧盆地性质与演化
2.
Transition of the Mesozoic-Cenozoic Tectonic Regimes and Hydrocarbon Accumulation in Western Ordos Region;
鄂尔多斯西缘中新生代构造体制转换与油气聚集
3.
The Mesozoic-Cenozoic Extensional Tectonics in Western Shandong Province;
鲁西中新生代伸展构造研究
5) 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
6) 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。
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