The front of south Qilian Mt. can be subdivided into two units:outcrop unit and basined unit, and strong tectonic activities, which controlled depositing process in Cenozoic and distribution of present Mesozoic systems, have occurred in Late Mesozoic in this area.
南祁连山前区可以分为露头和盆地区两个不同的大地构造单元，本区晚中生代构造活动强烈，控制了新生代的沉积过程和现今中生界残余层序的分布。
And Aimunike Mt, are focused; while in basined area, maps of residual Mesozoic thickness are mainy used, and Saishitengnan depression and Mahai uplift at the south of of Saishiteng Mt. and Aimunike Mt. are focused.
盆地区主要利用中生界残余厚度图的分析方法，研究区集中在赛什腾山-埃姆尼克山南侧的赛什腾南部凹陷和马海凸起地区。
Most extensional structures since late Mesozoic in West Shandong Rise, such as normal faults, developed on the base of the Mesozoic thrust fault`s negative inversion. The extensional structures inherited the characteristics of earlier structures and they appeared new active characteristics in new structure stress field.
鲁西隆起伸展构造是晚中生代以来发育的，如正断层，多是中生代逆断层负反转形成的，既继承了早期构造特征，又在新的构造应力场条件下，出现了新的活动特点，造成构造活动的多期性和方向上的多变性。
Dated from Proterozoic to Mesozoic, they have poly-circle characteristics, found from one tectonic circle to another, which is very rare in the worldwide orogens. This reveals that the orogen and stable area of the world, the mantle and crust states of the Proterozoic and Phanerozoic are different in tectonic evolvement and dynamic process and that the rapakivi granite of the Qinling-Kunlun is a kind of orogenic granite different from the stable area of the Proterozoic.
它们出现在每一个大的造山旋回晚期，即向另一个构造旋回的转折期，这在世界造山带中是十分罕见的，反映出世界上造山带与稳定区元古宙和显生宙的地慢与地壳状态是不一样的，有着不同的构造演化历史和动力学过程，表明秦岭－昆仑地区的环斑花岗岩是一种有别于元古宙稳定区的造山型环斑花岗岩。
The tectonic evolution of Mesozoic basin may be divided into Indosinian movement, Yanshan movement and Himalayan cycles.
结合中生代五期岩浆侵入和四期火山喷发活动，将中生代盆地演化分为印支、燕山、喜山三大旋回。
Lithologic character of Eogene syste is interbedded sandstone and mudstone primarily, including the thin layer oil shale, Neocene- Quaternary system is set of rivers deposits. Based on this, through the reaserch of ateral correlation and distribution characteristics of every structural layers show that: Paleozoic synthem overall thickness of relatively stable. The residual thickness of Mesozoic synthem is difference in the horizontal, Residues in the horizontal thickness of greater difference, to the greatest thickness achieve to 4500m. Eogene syste has obviously fault depression basin deposition characteristic, the thickness of many sags achieve to 3000 m, from Neocene, the stratum crosswise mop tended to be stable.
在此基础上，通过对各构造层横向对比以及展布特征的研究表明，古生界构造层整体厚度相对稳定，冷武-奥陶系残留厚度在1200m左右，石炭-二叠系残留厚度在800m左右；中生界构造层残留厚度在横向上差异较大，最大厚度达到4500m，其中，下-中三叠统仅发育于南部小部分地区，最大厚度在1000m以上，侏罗系-下白垩统整体具有南厚北薄的展布特征，南部冠北洼陷厚度最大，达到3500m；新生界古近系具明显的断陷式盆地沉积特征，多个洼陷厚度在3000m以上，新近纪以后地层横向展布趋于稳定。
Darwinopterus is a pterosaur, a member of the group of reptiles that soared above the landscape for much of the Mesozoic era.
Darwinopterus 是一只翼龙，这是大多数时间翱翔在中生代天空中的一类爬行动物。
Jinhuo fracture zone lies between Taihang shan block uplift and Qinshui depression, developed from a stage of thrusting in Mesozoic to a stage of tectonic inversion in Cenozoic.
位于太行山块隆和沁水块坳的晋获断裂带，经历了中生代逆冲推覆和新生代反转伸展的构造演化进程。
By above research, the following results are obtained.(1)The extracting module of aero-radioactive thematic information is integrated with ENVI, the remote sensing image processing software; (2) Based on the IDL, the computer program modules extracting following uranium thematic information have been developed, including initial uranium contents, active uranium contents, uranium migration coefficient, uranium information strengthen, uranium D-value and variance Ratio etc, al. Some of kalium special information extracting modules are also developed; (3)Based on the IDL, the aero-radioactivity information multi-parameter focus analysis module is developed; (4) It is proposed that a lots of phenomenon of uranium immigrating exist in Keping-Kuche are in the Neocene period. Because of the uranium pre-enrichment, the areas with high uranium content were formed in Neozoic and Quaternary. The above migration uranium are also the abundant source for uranium ore-forming in favorable strata of Mesozoic and Cenozoic system; (5)There are obvious uranium immigrating and enrichment in Eastern Portion of Keping Block Uplift, Yinate-Laolongjiang, and Qidaoban-KuChe.
通过上述研究，取得了如下成果：(1)实现了航放专题信息提取模块与ENVI遥感图像处理软件的无缝集成；(2)基于IDL语言开发了初始铀含量、活性铀含量、铀迁移系数、铀信息增强、铀差值方差比等航放铀专题信息，钾专题信息提取处理程序；(3)基于IDL语言开发了航放信息多参数聚焦分析处理程序；(4)发现柯坪-库车地区在晚第三纪开始出现了大量的铀迁移富集现象，不仅使上第三系、第四系沉积时因铀的预富集而形成铀含量高场区，而且也为研究区中新生代有利目的层的铀成矿提供了铀源条件；(5)研究认为，研究区柯坪断隆东段，英阿特-老龙江，七道班-库车等三个区块存在明显的铀迁入富集。
It was emplaced during exhumation of Mesozoic high pressure and ultrahigh|pressure metamorphic rocks in the Dabie orogen, central China.
它是在大别造山带中生代的高压超高压变质岩剥露过程中侵位的。
In the Mesozoic of the Well Wei 77-3 and Wei 77-4, some middle-lower Triassic fossils were discovered in some cores, which is about 235Ma by isotopic age analysis. It provides evidence for cognizing Mesozoic stratum of Dongpu depression as middle-lower Triassic.
东濮凹陷中生界地层时代归属长期不清，在卫77-3、卫77-4井中生界岩芯中发现了属于中下三叠统的宽肋粉、二肋粉等代表性化石，岩心同位素年龄分析在235Ma左右，确定了东濮凹陷中生界地层属中下三叠统。
Its main aims include:(1) understanding the magmatic processes of the volcanic rocks and their petrogeneses; (2) discussing the possible enrichment processes induced by subduction of continental slab; (3) providing geochemical constraints on the nature of lithosphere (including the subcontinental lithospheric mantle and lower crust) of the different tectonic units confined by the major faults across the belt; and (4) geochemical comparison of the lithosphere in an attempt to define the possible boundary between the North China and Yangtze Blocks during Mesozoic time.
中文摘要：项目开展了穿越苏鲁造山带南北向晚中生代火山岩及相关火成岩的廊带剖面(包括苏鲁带的胶东、青岛、滁州和下扬子地区的溧水盆地)的地球化学研究，理解各区块晚中生代岩浆作用过程和成因，探索大陆俯冲作用的地幔富集过程以认知各主要断裂围限地区的岩石圈性质；通过对比不同地区的岩石圈性质来限定苏鲁地区华北与扬子陆块的中生代碰撞边界。
Synthesized researches on biotic evolution, alternation and accurate chronological dating, taphonomy of vertebrate or invertebrate fossils and elemental or isotopic geochemistry of bones of fossils and sediments, i. e., HBCNOS and COSr, could help us to well understand the biotic and environmental response to the geological events on the Earth surface system and reconstructed the palaeogeography, palaeoecologic environment and palaeoecosystem of the Late Mesozoic, North China.
陆地生物群分布、演化、更替与精确定年，脊椎无脊椎生物埋葬特征，生物演化速率、消长关系和生物群更替的形式和性质，以及脊椎动物骨骼、牙齿的常量、微量元素、H-B-C-N-O-S 和C-O-Sr等地球化学特征的研究可以恢复和重建古地理、古生态环境和古生态系统。
Surprisingly, however, the new ligament-based force balance system appears to have evolved more gradually in Mesozoic fliers.
奇怪的是，不过，新的韧带为基础的力量平衡系统似乎已经逐渐演变更在中生代的传单。
Recent years, a lot of continental tight and supertight marginal oil fields were discovered in the Mesozoic basins of North Liaoning and Nei Monggol, among which Majiapu, Liao-1 district and Bai 3-4 district are three typical tight and supertight oil fields.
近年来发现辽北及内蒙中生代盆地存在众多陆相低渗、特低渗边际油田，马家铺、廖1块和白3－白4块3个低渗、特低渗油田就是典型代表。
The ultimate extinction of the dinosaurs 6300 years ago in the Mesozoic and Cenozoic Tertiary Paleocene.
恐龙最终灭绝于6300万年前的新生代第三纪古新世。
However, the extensive Mesozoic metamorphism and magmatism have been weakly related to lithosphere delamination. Based on a comprehensive review on research results of metamorphic rocks, the authors argue that the formation and exhumation of UHPM (ultra|high pressure metamorphite)experienced two stages, i. e., cold slab subduction and exhumation during 240～200?
构造地质研究、地球物理探测和地球化学分析等都已揭示东秦岭-大别造山带曾在中生代发生岩石圈拆沉，但有关中生代变质作用和岩浆活动与岩石圈拆沉的内在联系研究却较为薄弱。
Organic matter, pH, cation exchange capacity and contents of potassium, sodium, magnesium, copper, zinc, manganese, cobalt, iron, selenium, iodin and fluorin were determined of rock and soil samples from six main geological background areas within the main ruminant production base, in Yunnan Province, China. Results showed: 1 the red earth area of Paleozoic basalt and red earth area of carbonate the highest; the yellow-red earth area of mixture of carbonate, clasolite and basalt follows, except for its content of Co, which is relatively lower; and the purple earth area of Mesozoic clasolite, the yellow-red earth area of clasolite and the dark red earth area of Precambrian metamorphite are the lowest
对云南省反刍动物生产基地所属的6个主要地质背景区的土壤和岩石样品的K、Na、Mg、Cu、Zn、Mn、Co、Fe、Se、I和F元素及土壤的有机质、阳离子交换量和pH进行测定分析，结果表明：晚古生代玄武岩红壤区和碳酸岩盐红壤区土壤各种矿质元素都比较高，有机质含量与CEC都较高，特别是Ⅴ区最为显著；碳酸岩盐、碎屑岩和玄武岩混合型黄红壤区除了Co含量较低外，其他元素含量都居中等或偏上水平，有机质含量与CEC仅次于第1类背景区；碎屑岩紫色土区、变质岩赤红壤区和碎屑岩黄红壤区大多数矿质养分相对都比较低，有机质含量与CEC最低。
Diagnosis: The first Mesozoic bird found in Hebei Provicne. Different from Confuciusornis by smaller size, sharp teeth, well-developed sternum, carpometacarpus unfused and three wing claws present.
基本特征：是河北省发现的第一块中生代鸟类化石，它与孔子鸟不同之处有，个体较小，颌骨有锋利的牙齿，胸骨发育，腕掌骨不愈合，指骨仍有三个指爪。
The bimodal calc-alkaline rock belt consisting of gabbroic -granite may be regarded as a mark of Late Mesozoic large -scale extention tectonics in SE-China.
闽东南辉长岩-花岗岩的双模式钙碱性岩带可作为中国东南部晚中生代大规模拉张构造运动的标志。