打开新生成的类，将它的构造函数修改为public类型。
Open up your newly created class, and change its constructors to public type.
这令Annotation构造器能够根据J2Cbean和数据绑定文件中的所有的doclet Tag在方法体中重新生成代码，并且与工程同步。
This is to allow the Annotation builder to regenerate the code in method body based on all the doclet Tags in the J2C bean and data binding file, and to synchronize the project.
拷贝构造函数是一种特别的构造函数，用于复制已经存在的对象到新生成的对象，这是一种高效的方式。
The copy constructor is a special kind of constructor which creates a new object which is a copy of an existing one, and does it efficiently.
新生代构造现象既是中生代时期构造作用的延续，也是始新世以来复杂应力环境作用的结果。
The tectonic phenomena happened in the Cenozoic are caused by both of the continuity of the Mesozoic tectonic processes and the complexity of Cenozoic stress field.
具有工业意义的油气田均位于构造隐性急变带与中新生代盆地的立交地段。
The most of oil fields with industrial index are also located at the cross districts between basin and tectonic recessive geochemical boundaries.
从渤海湾盆地的中、新生代构造演化分析，渤海湾盆地是一个新生代早第三纪始新世形成的走滑拉分盆地。
According to the analysis of Mesozoic and Cenozoic tectonic evolution, Bohai Bay basin is a strike slip pull apart basin formed in the Cenozoic Eocene epoch.
深部构造与表层构造关系主要为构造继承，但也有构造新生。
The deep structure and surface structure are mainly of the tectonic inheritance, and also have new characters of tectonics.
晚白垩纪后，构造变形表现为一系列重新活动的基底断裂和新生断裂，褶皱构造简单。
After late Cretaceous, structural deformation shows a series of movable basement fault again and new's fault. The fold structure is very simple.
中国早、晚古生代、中生代和新生代成煤期的大地构造性质，在各个地区可有不同。
The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.
南沙海域新生代发生的多次构造运动既是盆地形成的主要原因，也是控制局部构造形成和发育的主要成因。
There are several construct movements at the southern part of south China Sea that are the main reason of basin formation and Local Structures forming and developing.
断裂和断块构造是南海北部陆缘新生代构造作用的基本特征。
Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic.
经长期构造演化于新生代转变为转换断层。
Through long terms of tectonic evolutions it changed into a transform fault in the Cenozoic era.
中生界与新生界主要是岩性圈闭与构造圈闭，而古生界的主要圈闭是断块潜山圈闭。
Lithology traps and structural traps are mainly found in Mesozoic and Cenozoic strata, while fault block-buried hill traps are primarily in Paleozoic strata.
本文对晚新生代贵州喀斯特地貌演进的三大控制因素 ，即地质基础、新构造运动及挽近气候波动进行了分析论证。
In this paper, three determined factors influencing on the evolution of karst geomorphology of upper Cenozoic in Guizhou, e.
新生代地堑构造是华北地区最普遍和最有特征的构造。
Cenozoic graben structure is the most general and characteristic tectonic in North China.
临清坳陷东部新生代盆地的变换构造类型以调节构造为主，传递构造不多见。
Different types and structure styles of the Cenozoic transition structures in the east of Linqing depression are examined.
新生代时，岩石圈中出现了物质的重新分配与调整，产生了地史上最为显著的构造隆升。
During Cenozoic, the most remarkable tectonic uplift in geologic history appeared as the result of material redistribution and adjustment in lithosphere.
笔者在盆山构造及构造地貌发育的基础上，对研究区构造和沉积记录进行了分析，进而探讨了新生代以来河西走廊与北祁连山的耦合关系。
The coupling relationship between the Hexi Corridor Basin and North Qilian Mountains is discussed in terms of tectonic and depositional records in the study areas from the Cenozoic onwards.
结合区域火山活动和构造演化认为，该滑动构造为伸展背景下的掀斜断块型，其滑动时间为白垩纪—新生代。
Based on volcanic activities and tectonic evolution, it is suggested that the tilted fault block, sliding structures in extensional setting should be developed in Cretaceous to Cenozoic age.
进入新生代喜马拉雅期，本区的构造格局发生了重大变革，即由原来的NW—SE向挤压构造应力场变为ne—sw挤压构造应力场。
In the Cenozoic Himalayan period, great changes took place in the tectonic framework in the study area, i. e. the original NW-SE compressional stress field changed into a NE-SW one.
这一研究为了解华南内部中新生代以来陆下岩石圈地幔的属性以及构造演化提供了重要的信息。
This study will provide important information for well understanding and probing into the nature and tectonic evolution of sub-continental lithospheric mantle since the Mesozoic-Cenozoic.
基于大陆根柱构造概念，讨论了新生代以来中国大陆岩石圈尺度的大地构造分区。
Based on the concept of continental roots plume tectonics, geotectonic units of China continent on a lithospheric scale since Cenozoic are discussed in this paper.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
青藏高原新生代伸展地堑构造是高原经历早期地壳强烈缩短变形之后，在深部动力学机制作用下快速隆升的产物。
The Cenozoic extensional grabens on the Qinghai-Tibet plateau are the product of rapid uplift of the plateau caused by the deep dynamic mechanism after earlier strong crustal shortening.
形成这一构造格局的主要动力来自新生代以来南海的拉张作用以及澳洲板块南北向的推挤作用。
The main driving forces for generating the fault structure pattern are the seafloor spreading of the South China Sea and the northward subduction of the Australian Plate.
新生代盆地构造和沉积分布特征表明渤海湾盆地是一个中、新生代叠合盆地。
The characteristics of structure and depositment in this Mesozoic and Cenozoic time show that Bohai basin is a Mesozoic and Cenozoic composite basin.
一些于前地槽、地槽阶段形成的褶皱构造体系所控制的内生金矿产，在形成时代上也属于中-新生代。
Some endogenetic gold deposits controlled by the fold systems which situated in the pre geosynclinal and the geosynclinal stages are formed in the Meso Cenozoic eras also.
新生代以来，沾化凹陷岩浆活动(构造-热事件)十分强烈，且这种岩浆活动受基底断裂的控制。
Since Cenozoic period, the magmatic activity (tectonic-thermal event) in Zhanhua Sag is very strong and it is controlled by basement fracture.
新生代以来，沾化凹陷岩浆活动(构造-热事件)十分强烈，且这种岩浆活动受基底断裂的控制。
Since Cenozoic period, the magmatic activity (tectonic-thermal event) in Zhanhua Sag is very strong and it is controlled by basement fracture.
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