1) tectonic evolution
构造变格
1.
Since the Indosinian epoch,under a condensing tectonic environment compressed from3 sides,the Chinese continent has experienced 4 stages of tectonic evolution:T3-J2,J3-K1,K2-E,and E3/N-Q,resultingin corresponding basin prototypes along both sides of the Qinling-Dabie orogenic belt.
印支期以来,中国大陆在三面受挤的缩合构造环境下,经历了4期构造变格作用(T3—J2,J3—K1,K2—E,E3/N—Q),秦岭—大别两侧发育了相应的陆相盆地原型,并形成了复杂的原型并列叠加关系。
2.
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) structure pattern
构造格局
1.
According to the characteristic of Bouguer gravity and regional gravity anomaly, the authors worked out a plot of structure pattern in the crystalline base of the basin.
根据虎林盆地布格异常和区域场特征,编制断裂及基底构造格局图,将盆地划分为条带状的3个隆起区和2个凹陷区,研究区可划分为近NE向、NEE向和EW向8条断裂。
3) structural framework
构造格局
1.
the western rifted zone, the central uplifted zone and the eastern depressed zone, and each zone is distinctive in structural framework and has itself source rocks.
东海盆地自西向东可分为 3个带 ,即西部断陷带、中部隆起带和东部断坳带 ,其构造格局各具特色 ,并且均有自身的烃源岩。
2.
In the paper the authors give out the major outcome obtained by using magnetotelluric sounding in the Dongting depression in Hunan Province, and carefully analyse and deduce the regional structural framework, electrical property structure of the depths and the distribution character of high conductivity layers in the earth's crust and the earth's mantle of the Dongting depression in Hunan.
详细分析、推断了洞庭地区的区域构造格局，深部电性结构及壳、幔高导层的分布特
3.
The deep and shallow structural frameworks are quite different in the Qaidam Cenozoic basin according to a comprehensive interpretation of seismic and non-seismic data.
应用柴达木盆地地震、非地震资料进行综合解释研究发现,新生代盆地深、浅层构造存在较大差异,盆地沉积在不同时期受到不同构造格局的控制。
4) tectonic framework
构造格局
1.
Late Paleozoic tectonic framework and evolution in the Jiabaishan area, Qoltag, eastern Tianshan Mountains, Northwest China.;
东天山觉罗塔格地区夹白山一带晚古生代构造格局及演化
2.
Stratigraphic and paleobiogeographic affinities between different tectonic units in northwestern China-With a discussion of the tectonic framework of northwestern China.;
中国西北地区各构造单元之间地层和生物古地理的亲缘关系——兼论西北地区构造格局
3.
Mesozoic tectonic framework and evolution in the central segment of the intraplate Yanshan orogenic belt;
燕山板内造山带中段中生代构造格局与构造演化
5) structural framework
构造格架
1.
Growth structural framework and hydrocarbon accumulation in Cenozoic in the west Qaidam Basin, Northwest China;
柴达木盆地西部新生代生长构造格架与油气聚集
2.
From an analysis of superposition structure, a detailed subdivision of the Meso Cenozoic ductile brittle deformation episodes and mechanism in the Dalian area is made and the structural framework is redetermined for this period.
从叠加构造解析入手 ,详细划分了大连地区中、新生代的韧—脆性变形构造期次、变形机制 ,重新厘定了该区的中、新生代构造格架 ,并进行了区域动力学问题的讨论。
6) Structural pattern
构造格局
1.
It controled the structural pattern in Palaeozoic Era.
地质、地球物理测深研究成果揭示新疆东部、甘肃西部存在两个世代、两种不同的断裂体制:深部断裂体制,形成于古生代,主要反映板块碰撞-对接前板块之间或板内不同块段之间的离散与聚合,控制古生代的构造格局;浅部断裂体制,形成于华力西晚期至中新生代,主要反映板块碰撞-对接后壳内强烈水平挤压,控制中新生代构造格局或逆冲-推覆-滑脱构造。
补充资料：构造实变函数
构造实变函数
constructive function of a real variable
构造实变函数{~加dve血.面皿试a比址银‘able;取幻即cTP外汀”..翻中如圈刀.月d七.扣，呱.OTo”e碑M姗-HO印]，均填甲攀(cons‘ruCtive fun以ion) 一元或多元函数论中的一个概念，用于构造数学(constructive mat十lemati“).它是由A.A.MaPkOB引人的，可以作为构造度量空间中算法算子概念的一个特例.亦见构造分析(constructive analysis);构造度t空间(constructlve metrie sPa优)·
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