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tectonic style    
相关语句
  构造样式
    TECTONIC STYLE AND DEFORMATIONAL SEQUENCE OF DABIE METAMORPHIC TERRANE
    大别变质地体的构造样式及变形序列
短句来源
    ANALYSIS ON CONTROL OF TECTONIC STYLE TO PETROLEUM IN THE QAIDAM BASIN
    柴达木盆地构造样式控油作用分析
短句来源
    FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
    伊通地堑断层系统与构造样式
短句来源
    Tectonic style and deformation difference of granite bodies in the opening-closing tectonic setting
    开合构造环境下花岗岩体的构造样式与变形差异
短句来源
    3、Tectonic style of the orogenic-belt uplift is very complicated,and is markedby the growing of a large number of thrusting rupture and faulted block.
    3、造山隆起带构造样式较复杂,发育大量的逆冲断裂与断块体;
短句来源
  构造样式
    TECTONIC STYLE AND DEFORMATIONAL SEQUENCE OF DABIE METAMORPHIC TERRANE
    大别变质地体的构造样式及变形序列
短句来源
    ANALYSIS ON CONTROL OF TECTONIC STYLE TO PETROLEUM IN THE QAIDAM BASIN
    柴达木盆地构造样式控油作用分析
短句来源
    FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
    伊通地堑断层系统与构造样式
短句来源
    Tectonic style and deformation difference of granite bodies in the opening-closing tectonic setting
    开合构造环境下花岗岩体的构造样式与变形差异
短句来源
    3、Tectonic style of the orogenic-belt uplift is very complicated,and is markedby the growing of a large number of thrusting rupture and faulted block.
    3、造山隆起带构造样式较复杂,发育大量的逆冲断裂与断块体;
短句来源
  构造样式
    TECTONIC STYLE AND DEFORMATIONAL SEQUENCE OF DABIE METAMORPHIC TERRANE
    大别变质地体的构造样式及变形序列
短句来源
    ANALYSIS ON CONTROL OF TECTONIC STYLE TO PETROLEUM IN THE QAIDAM BASIN
    柴达木盆地构造样式控油作用分析
短句来源
    FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
    伊通地堑断层系统与构造样式
短句来源
    Tectonic style and deformation difference of granite bodies in the opening-closing tectonic setting
    开合构造环境下花岗岩体的构造样式与变形差异
短句来源
    3、Tectonic style of the orogenic-belt uplift is very complicated,and is markedby the growing of a large number of thrusting rupture and faulted block.
    3、造山隆起带构造样式较复杂,发育大量的逆冲断裂与断块体;
短句来源
  构造样式
    TECTONIC STYLE AND DEFORMATIONAL SEQUENCE OF DABIE METAMORPHIC TERRANE
    大别变质地体的构造样式及变形序列
短句来源
    ANALYSIS ON CONTROL OF TECTONIC STYLE TO PETROLEUM IN THE QAIDAM BASIN
    柴达木盆地构造样式控油作用分析
短句来源
    FAULT SYSTEM AND TECTONIC STYLE OF THE YITONG GRABEN
    伊通地堑断层系统与构造样式
短句来源
    Tectonic style and deformation difference of granite bodies in the opening-closing tectonic setting
    开合构造环境下花岗岩体的构造样式与变形差异
短句来源
    3、Tectonic style of the orogenic-belt uplift is very complicated,and is markedby the growing of a large number of thrusting rupture and faulted block.
    3、造山隆起带构造样式较复杂,发育大量的逆冲断裂与断块体;
短句来源
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  tectonic style
Similarly, the details of plate tectonic modalities (plate size, plate motion rate, plate thickness, tectonic style, irregular crustal growth, etc...) were different of modern plate tectonics.
      
The tectonic style of a terrestrial planet depends strongly on the mechanisms of heat release from the mantle through the lithosphere to the surface.
      
Today one of the main questions standing before geology of Venus is comprehension of tectonic style on surface of this planet.
      
These factorsinfluence the mechanical properties of the lithosphere across thediscontinuity, and ultimately the tectonic style of the NTD that can besupported.
      
Swath bathymetry and sidescan data, together with seismic reflection and geopotential data obtained during the GEODYNZ-SUD cruise, showed major changes in tectonic style along the margin.
      
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According to the theory of Diwa, through a detail study of geotectonic characteristies, it comes to a conclusion that North Xinjiang, developed from geosyncline and platform, has been in diwa stage now. According to diwa metallogenic theory, it suggests that there are three oil formation periods in this area: geosyncline, platform, and diwa. All the oil formation periods have oil and gas reservoirs of industrial significance. It also suggests the oil prospect of this region after a study of source-reservoir-seallng...

According to the theory of Diwa, through a detail study of geotectonic characteristies, it comes to a conclusion that North Xinjiang, developed from geosyncline and platform, has been in diwa stage now. According to diwa metallogenic theory, it suggests that there are three oil formation periods in this area: geosyncline, platform, and diwa. All the oil formation periods have oil and gas reservoirs of industrial significance. It also suggests the oil prospect of this region after a study of source-reservoir-seallng beds in different oil formation periods and its combined characteristics, different geotectonic stages tectonic styles and reconstraction and Superposition of later teetonism to the old.

本文以地洼学说的观点,详尽地分析了北疆西部的大地构造特征,明确指出本区在大地构造进程中,经历过地槽阶段、地台阶段,现阶段属地洼阶段。根据地洼成矿理论,指出本区存在着三个成油期,即地槽期、地台期、和地洼期。每一成油期都存在有工业价值的油气藏。根据不同成油期生、储、盖及其组合特征,根据不同发展阶段的构造型相特点,以及后一阶段对前期构造的改造,叠加,指出了含油远景有利区。

Tectoncally,the area studied is located in the northeastern part of the North China Platform, which is one of the typical regions for researching the evolution of Early Precambrian crust.A detailed study and analysis of various structural elements in the Early Precambrian rock groups of the area reveal that these rocks have suffered to Polyphase deformation.Four tectonic cycles (i.e. I . II.III . IV) have been distinguished, and each of them contains at least two episodes of deformation.However,the vari-arion...

Tectoncally,the area studied is located in the northeastern part of the North China Platform, which is one of the typical regions for researching the evolution of Early Precambrian crust.A detailed study and analysis of various structural elements in the Early Precambrian rock groups of the area reveal that these rocks have suffered to Polyphase deformation.Four tectonic cycles (i.e. I . II.III . IV) have been distinguished, and each of them contains at least two episodes of deformation.However,the vari-arion of tectonic styles shows a tendency of changing from planar to linear structures.The dominant structure of F1 fold controled the distribution of ore-bodies, and F2 and F3 folds exerted some modifications on these ore-bodies.Fold interference patterns of various scales are ubiquitous throughout the region, many of which belong to type 2 and type 3 and the mixed type of type 2 and type 3 of Ramsay's classification.Mullion structures observed always occur at the hinge of folds, so they are excellent indicators for folds.In addition to the discussion on tectonic sequence and style of each tectonic cycle,the deformation history of the Early Precambrian rock groups and the configuration of regional structure have also bean refer ed in the paper.

研究区为地台古老变质群典型出露区之一,详细地质、构造研究对探讨地壳早期演化规律、鞍山铁矿床的成因及构造对矿体的控制规律等,都是十分重要的。

Based on applying the techniques of structural analysis to rocks involved in the so-called "Yingtaoyuan Formation" near Anshan city, Liaoning province, structural sequence and thus the tectonic style of this formation have been discerned and clarified. Rocks belonging to the "Yingtaoyuan Formation" have undergone at least three phases of deformation during Proterzoic time. The first phase of deformation produced folds ranging in size from intrafolial to regional scale and generally exhibiting tightly appressed...

Based on applying the techniques of structural analysis to rocks involved in the so-called "Yingtaoyuan Formation" near Anshan city, Liaoning province, structural sequence and thus the tectonic style of this formation have been discerned and clarified. Rocks belonging to the "Yingtaoyuan Formation" have undergone at least three phases of deformation during Proterzoic time. The first phase of deformation produced folds ranging in size from intrafolial to regional scale and generally exhibiting tightly appressed to isoclinal forms of nearly N-S trend. F1 folds have a best development and exercise the major control on the disposition of rock units within entire area. S1, a newly formed planar element which is an axial plane to F1 folds, is defined by the preferred orientation of platy minerals such as,mica and chlorite in pelitic rocks and by parallel banding in ore-bearing quartzite. It shows transposition relationship with preexisting So, the origional bedding of rocks. Linear structures including boudins, mullions and Si/So intersections are found in various rock types. Mullions are always occurred in the hinge protions of folds (particularly in antiform) and this may be taken as an indication to identify folds in thick-bedded and even massive rocks. Structures by which the second phase deformation was denoted are S2, F2 and L2. S2 is a set of typical crenulation cleavage that overprinted on an anisotropic background of rocks which already contained earlier structures S0, S1 and F1 etc.. It is an axial plane to F2 folds, a series of folds of mainly mesoscopic in size except those distributed in the Yanqianshan domain. Fine wrinkles, the surface expression of S2/S1 intersections, labelled L2, are widely distributed on S1 (≈S0) surface within pelitic rocks and run parallel to axial trends of folds nearby. Third phase deformation is marked by the spasmodically developed kink-bands. All of these indicate a general evolution tendency of decrease in both metamorphic temperature and plasticity of rocks during this tectonic cycle. On the basis of considering the geometrical homogeneity of the S1 fabric, 9 domains were divided throughout the area occupied by this formation. Data obtained from field survey have been plotted on equal-area stereogram (lower hemisphere) for each domain. Preferred orientation and trend determination of the ambiguous fabric patterns are determined by means of computer treatment using the eigenvalue method. By comparing the structural sequence and tectonic style in the "Yingtaoyuan Formation" to those in the underlying granulite association of the Archean Anshan Group, it is obvious that a great difference exists between these two rock units and that it is improper to regard the "Yingtaoyuan Formation" as one unit of the Archean Anshan Group as was proposed previously by many geologists. However, there is a great resemblance between this formation and the overlying Liaohe Group (Upper Proterozoic) in two aspects, i.e. the structural sequence and the metamorphic facies, so it is reasonable to correlate the time of this formation to Ferrian of Early Proterozoic.

本文区分了“樱桃园组”岩石在元古主构造旋回的三幕变形,详细描述了各幕SFL组合和按区段进行了投影。主变形幕D_1的构造最发育,F_1控制着本区的岩性分布。构造序列及样式变化显示由高塑性向脆性的变形格式。本组与下伏的太古鞍山群变粒岩在构造序列、样式和变质相上都有显著差异,过去许多地质学家把二者混划为一个单位,统名“鞍山群”,属太古宙。但本组与上覆的辽河群(上元古)的构造样式和变质相却相似,故其时代相当于早元古Ferrian期。

 
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