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The orogenic strata have following characteristics: During the subduction and intracontinental orogeny, the strata experienced dramatic tectonic migration and mixing, resulting in various tectonic features. A short sequence usually composed of tectonic slices of various origins, times, deformations and metamorphisms, and scales. The original sequence was badly destroyed. The extant fragments of orogenic belt usually took form as melanges, especially the accretion complex wedge generated in subduction zone, which is contrary to the Law of Superposition. The original location of the accretion is also contradicted with the Law of Original Horizonality, because the accretion is oblique with high degree. Marine rocks, volcanic rocks of continental margin and metamorphic rocks were well-developed in the orogenic belt, especially ultra-basic, basic rocks were wide spread and were intensely metamorphosed, accompanied by metamorphic slices returned from hundred kilometers underground with ultra-high pressure and magma movements during syn-orogeny and post-orogeny, thus formed the colorful landscapes.

造山带非史密斯地层构成具如下独特性和复杂性:造山带在俯冲碰撞和陆内造山阶段,发生过强烈的构造搬运和构造混杂,构造形迹多样化,垂直不长的地层体往往是众多不同来源、不同时代,不同变形变质程度,不同大小的各种构造岩片拼贴体,地层原始层序被严重肢解、破坏;尤以产于俯冲带的俯冲增生杂岩楔的原始形成方式与史密斯地层学的&层序叠覆律&老下新上的顺序正好相反,其混杂岩增生方式是老的&片体&在上,新的&片体&阶段性拼贴在老的&增生片体&的斜下方,这种增生片体的原始位置亦与&原始水平律&相悖,即增生片体一般保持较高角度倾斜;在岩石类型和变质程度上,造山带海相和古陆缘火山岩以及变质岩普遍发育,尤其是超基性、基性岩系分布广泛,变质作用较强,伴有从百余公里以下深部超高压变质岩片的折返和同造山期与造山后期岩浆活动,构成极为复杂的地质景观。

Referencing to the internal and external documents, we have plotted the balanced evolutions for the various typical structures by computer, which is the first time at home; applied the balancing technique by computer to the representative structures in Sichuan Oil and Gas Basin, and also established the geological modellings on three different structural elements and their own balanced evocutions in Sichuan Basin.

借鉴国内外的资料,在国内首次用计算机绘制出各种典型构造的平衡演化剖面,并应用机制平衡技术对四川油气盆地内的代表构造作了详细的平衡计算,建立起四川盆地内三个不同构造单元的地质模型以及构造平衡演化剖面。

Applied the balanced cross-section technique to explain the characteristics of Kuqa rejuvenated foreland basin nappes and its structural shorten distance, and applied the structural triangle deposition bed discussed the time of structural deformation, that is structural deformation time in north older than in south area in Kuqa depression.

建立了库车再生前陆盆地6种局部构造变形的地质模型;利用平衡剖面技术解释了库车再生前陆冲断带,查明了构造变形特征和地层缩短量;研究了库车再生前陆盆地构造变形时间,探讨了前陆冲断带造山运动的特征和规律,指出库车前陆冲断带构造变形自北(25Ma)向南(2.5Ma)依次变新。

During early and middle Jurassic period, as a northern boundary, the fault zone controlled a seires of sedimentation of coal basins and magma activity. A lot of nappes developed during Ⅰ,Ⅱ and Ⅲ phase of the Yanshan movement. The strongest structural activity during the Yanshan movement is the Ⅱ phase, It had three pulsation and formed large-scale tectonic system with dextral strike slip.

早、中侏罗世,断裂带作为北界,控制了由西向东一系列煤系盆地的沉积作用和岩浆活动;在燕山运动的Ⅰ、Ⅱ、Ⅲ幕中分别形成了一系列逆冲构造;其中,以燕山Ⅱ幕构造活动最强,并至少经历了三次脉动作用,形成的逆冲构造不是由盆缘到盆内的&对冲&,而是受本断裂带限制,并以之为主滑面构成了区域上的大型右行走滑斜压式构造系统。

The tectonic setting in which they formed was affected and constrained by the Paleo-Asiatic tectonic domain in the setting of the peri-Pacific domain,rather than only resulted from the activity of the peri-Pacific tectonic mobile belt.

其形成时的构造环境应是在滨太平洋构造域背景下受古亚洲构造域的影响和限制,并非是滨太平洋构造活动带的单一活动所致。

Tectonic analysis of Pre-Carboniferous metamorphic stratum and structural foliation dating have shown that The Qinling and its vicinities had happened an important regional tectonic event -Caledonian event, this event represents early paleozoic closure of the Qinling ocean basin and continent-continent obliquely diachronous collision, so we also could reconstruct Caledonian Qinling orogenic belt's basic tectonic framework.

对北秦岭地区前石炭纪变沉积—火山岩地层系统进行构造解析,以及构造面理定年数据表明,秦岭及邻区志留纪至早泥盆世经历了区域性的重大构造事件,相当于加里东事件,该事件代表了秦岭早古生代洋盆闭合、陆—陆碰撞造山的造山事件,并可恢复加里东古造山带的基本构造格局。

Results of inversion show that pre-Tertiary deposition in Dongying depression is controlled with westnorth structures. Archaean group is the crystal basement of Dongying depression, which is a north steep and south gentle rift subsidence basin striking from eastnorth to near westeast, and the deepest position is up to 12000 m at the area of Xianhe and Xinzhen. The configuration of Ordovician of lower Palaeozoic system highly inherits that of Archaean group and both have a strong consistency. The configuration of Mesozoic inherits that of lower Palaeozoic system as a whole, but filling and local reconstruction are distinct, and the scope of Dongying depression has obviously decreased.

结果表明,东营凹陷前古近系沉积主要受北西向构造的控制,太古界构成东营凹陷的结晶基底,是一个北东转近东西向的北陡南缓的断陷,最深处位于现河、辛镇一带,可达12000 m;下古生界奥陶系构造具有很强的继承性,其构造格局与太古界有很强的一致性;中生界宏观上继承了下古生界的构造形态,但填平补齐和局部改造比较明显,凹陷范围明显缩小。

Based on analysis for paleostructural characteristics of above four areas,the paper proposed that there developed a series of paleostructure belts under the background of regional uplifting in latest Mesozoic at the front of south Qilian Mt,and those paleostructures are characterized by NWNNWstriked anticlines and synclines,whose wavelengths are 15~20 km and middlescaled. At the same time,the paper also points out that most areas in western China are lack of upper Cretaceous,which implies the existence of a broad Late Cretaceous plateau in central Asia.

通过这4个地区古构造特征的研究,提出南祁连山前区中生代晚期在区域性隆升的背景下,形成了一系列古构造带,古构造活动的特点是形成北西-北北西走向的背斜和向斜构造,这些褶皱的波长为15~20 km,为中尺度规模。

The study on structural pattern of plutons can reveal more information of regional deformation, provide us detailed information of structural evolution of orogenic belts, define the emplacement mechanism of plutons, and help to investigate the feedback relationship among magmatic activities, tectonism and deep processes.

岩体构造样式研究可以揭示更多的区域变形信息,可以提供造山带演化详细的构造演化信息,可以确定出岩体侵位机制,并进一步探讨岩浆活动与构造作用及深部过程之间的互反馈关系。研究花岗岩构造变形是花岗岩研究与大陆动力学研究的一个结合点。

With the help of these conditions, computer efficiently searches out many quasi-perfect and double quasi-perfect punctured binary array pairs. The relationships among perfect punctured binary array pair, quasi-perfect and double quasi-perfect punctured binary array pair is presented. Specially, when first and second dimension period of the punctured binary ar

定义了非周期屏蔽二元序列偶的自相关函数、屏蔽二元互补序列偶和最佳屏蔽二元互补序列偶,给出并证明了屏蔽二元互补序列偶的变换性质;和它存在的组合允许条件,用计算机搜索出若干最佳屏蔽二元互补序列偶;给出了屏蔽二元互补序列构造出新的屏蔽二元互补序列偶的四种构造方法;并且,给出了利用不同长度的二元互补序列和屏蔽二元互补序列偶构造出新的屏蔽二元互补序列偶的四种构造方法。

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