| 1. | The case shown in figure 56 corresponds to a dextral horizontal displacement along a vertical fault surface .
图56所示例子表示沿垂直断层面的右旋水平位移。 |
| 2. | In experiments ， an injection of cytoplasm from dextral eggs changes the pattern of sinistral eggs ， but an injection from sinistral eggs does not influence dextral eggs
用取自左旋卵子的细胞质进行的注射却不能影响到右旋卵子。 |
| 3. | In experiments ， an injection of cytoplasm from dextral eggs changes the pattern of sinistral eggs ， but an injection from sinistral eggs does not influence dextral eggs
在实验中，用取自右旋卵子的细胞质进行的注射，可改变左旋卵子的模式；用取自左旋卵子的细胞质进行的注射却不能影响到右旋卵子。 |
| 4. | 4 ) analyses boundary faults of the cenozoic longmenshan foreland basin , and thinks the basin boundary faults , being active fault , are thrust and dextral strike - slip . so the longmenshan foreland basin is dextral strike - slip foreland basin
4 )通过对新生代龙门山前陆盆地边界断裂的考察分析，认为盆地边界断裂具逆冲推覆及右旋走滑作用特点，为活动断裂。 |
| 5. | 5 ) quantitative analysis to the dayi conglomerate in the cenozoic longmenshan foreland basin has been carried out . the results indicate that the dextral strike - slip rate is 1 . 02 mm / a , the average sedimentary rate is 0 . 143 mm / a , and the average decline rate is 0 . 3mm / a
5 )对新生代前陆盆地大邑砾岩作定量分析，结果表明，大邑砾岩沉积时期，前陆盆地滑移量为1 . 02mm a ，沉积速率为0 . 143mm a ，平均沉降速率为0 . 3mm a 。 |
| 6. | K - ar age of an illite from alteration rock in the contact zone around lianhuashan porphyry is 38 . 6ma . with referencing to the main metallogenic period of yulong copper metallogenic zone and of ailaoshan gold metallogenic zone , it is suggested that the time of formation of deposits in the district studied is probably in a period of time from 38 . 6ma at earliest to 20ma at latest . this time is equivalent to the origination time of two important tectonic events , i . e . , lanping movement and the turning point when ailaoshan - red river fault turned from sinisteral into dextral
获得了莲花山岩体周围接触带蚀变岩中伊利石k - ar年龄38 . 6ma ，参考玉龙铜矿带和哀牢山金矿带的主要成矿期(分别为30ma左右及26ma ) ，厘定本矿集区成矿年龄下限为38 . 6ma ，上限为20ma ，与两次重要的构造事件?兰坪运动的起始时间及哀牢山?红河断裂由左旋转为右旋的时间相当。 |
| 7. | On the basis of detailed field work and structural analysis , this paper presents a new geometrical and kinematic data that reveal the staictural characteristics of qinglong fault zone . this fault zone is composed of numerical ew faults with an arrangement of dextral step pattern in the western part , and consists of maquanzi - datun fault and tumenzi - mingshui fault in the eastern part
本文通过较为详细的野外调查和室内研究，并结合前人的研究资料，以构造解析为指导思想，对断裂带的几何学、运动学特征进行了研究：青龙断裂带是由一系列近东西向的断层组合而成，断裂带西段呈明显的右行右列式分布，东段主要有马圈子?大屯断裂和土门子?明水断裂组成。 |
| 8. | Sxotf is recognized in the northern qaidam based on the analysis of structures of area . this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge , fault breccia and fault cleavage . fault hanging wall consists of sertengshan - xitieshan napple , which is distribution in dextral en echelon . fault footwall consists of youcangshan formation in neogene
本文在对赛什腾? ?锡铁山斜冲断裂详细地段构造解析的基础上，结合盆地的沉积特征、地球物理资料等对该斜冲断裂的几何学、运动学及形成时代进行了研究，论文着重探讨了赛什腾? ?锡铁山斜冲断裂的地质意义。 |
| 9. | It is believed that three northeast - striking dextral slip fault zones , i . e . the baxian - shulu - handan fault zone , the huanghua - dezhou - dongming fault zone , and the linyi - huanghekou fault zone , are the result of the tectonic transform of paleogene extending to neogene - quaternary laterally slipping of north china plain rift systems , which extend along the central axis of rifts and accord with the quaternary centers of subsidence as the main seismic structures within the rifts
认为坝县束鹿邯郸断裂带、唐山河间磁县断裂带和黄骅德州东明断裂带3条北东向右旋走滑断裂带为华北平原裂谷系从早第三纪伸展拉张作用进入晚第三纪第四纪走滑剪切拉张作用的产物，这3条断裂带分别位于3个北东向坳陷带中部，并构成了第四纪沉降中心，与营口潍坊断裂带起构成华北平原内的主要强震构造。 |
| 10. | Especially interesting is the serpentinous peridotite in this belt occurred as lense blocks of various sizes , and superimposed with other geological masses with faults , and in combine to constitute the mixture . system in the belt . five tectonic stage can be discerned in this area : ( 1 ) south - north ward overthrust ; ( 2 ) sinistral strike - slip ( 3 ) dextral strike - slip ( 4 ) south - north ward overthrust ( 5 ) northeast , northwest late stage fault
本区上述的结构构造特征先后经历了五期构造作用，依次为： ( 1 )南北向逆冲推覆； ( 2 )左行走滑； ( 3 )右行走滑； ( 4 )南北向挤压推覆； ( 5 )北东向、北西向晚期断裂； |
