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According to the characteristics of faults in planes and profiles, faults, basically NS striking, separate the diapir into west and east two blocks in the aspects of pressure system, gas-water boundary and hydrocarbon component.

通过对断裂系统及超压流体特征等诸方面的详细研究,结合区域构造演化,对断裂与超压流体的成因关系提出了新见解,揭示出断裂对超压流体的输导及超压流体对断裂的开启的相互作用。

It was suggested that the risk of active faults can be reasonably explained by the history of the faults and their occurrence period, while the risk of groundsill seismic liquefaction was examined in the field with penetration test.

活动断裂的危险性主要根据断裂的活动时期、断裂不同部位的活动性以及评估区距离断裂活动部位的远近程度进行评估。

It was suggested that the risk of active faults can be reasonably explained by the history of the faults and their occurrence period,while the risk of groundsill seismic liquefaction was examined in the field with penetration test.

活动断裂的危险性主要根据断裂的活动时期、断裂不同部位的活动性以及评估区距离断裂活动部位的远近程度进行评估。地震砂土液化判别采用现场标准贯入试验进行评估。

The mechanism of mixed fracture type as well as fracture criterion of different types have been discussed from the viewpoint of interface mechanics.

此外,还用界面断裂力学的方法分析和探讨了发生混合断裂的机制,以及不同断裂类型的断裂判据。

The result shows that the Coulomb failure stresses increased along the southwest and northeast segments of the Gonggacuo fault, the east and west segment of the Kengxiwar faults, the west segment of the Pulu fault, the west segment of the Lungmu Co—Bangdag Co, the Altyn Tagh fault and the western Kunlun thrust fault by 6.9×104 Pa, 4.4×103 Pa, 8.0×105 Pa, 2.8×103 Pa, 2.3×104 Pa, 5.7×103 Pa, 1.6×103 Pa and 1.1×103 Pa, respectively, decreased along the central segment of the Gonggacuo and Kengxiwar faults, the east segment of the Lungmu Co—Bangdag Co fault, the central segment of 〖JP2〗the Pulu fault, and the north segment of the Karakorum fault by 3.9×105 Pa, 5.8×105 Pa, 1.5×104 Pa,1.5×104 Pa and 1.1×103 Pa, respectively.

结果表明,库仑应力在贡嘎错断裂的西南段和东北段、康西瓦断裂东段和西段、普鲁断裂西段、龙木错-邦达错西段、阿尔金断裂和西昆仑山前逆冲断裂增加分别达6.9×104 Pa、4.4×103 Pa、8.0×105 Pa、2.8×103 Pa、2.3×104 Pa、5.7×103 Pa、1.6×103 Pa和1.1×103 Pa,而使得贡嘎错断裂中段、康西瓦断裂中段、龙木错-邦达错东段、普鲁断裂中段和喀喇昆仑北段断层上的库伦破裂应力减小分别达3.9×105 Pa、5.8×105 Pa、1.5×104 Pa、1.5×104 Pa和1.1×103 Pa。

According to the forming reasons, the types of capital chain rupture can be divided into six: The stock increasing type, the value foam type, the capital operation type, commission financing type, capital sponsion type and affiliated parts occupies type.

根据形成"资金链"断裂的原因,将其划分为:库存增加型"资金链"断裂、价值泡沫型"资金链"断裂、资本运做型"资金链"断裂、委托理财型"资金链"断裂、资金担保型"资金链"断裂和关联方占用型"资金链"断裂六种类型。

Based on the analysis of vertical open degree of fault and its influence factors in active period ,a method judging vertical open degree of the fault in active period was set up by the angle between the orientation of maximum principal compressive stress and the strike of the fault.

在分析断裂活动时期垂向开启程度及其影响因素的基础上,利用最大主压应力方向与断裂走向之间夹角的大小,建立了一套断裂活动时期垂向开启程度的判别方法,将其应用于海拉尔盆地贝尔凹陷布达特群潜山4条主要源断裂的研究中。

Furthermore, the computational results indicate that the surface displacement fields varies with the distance form the fault, and the vertical displacement fields show strong inhomogeneity, in which largen displacement focuses on the ends of fault.

同时通过计算揭示了断裂错动过程中离断裂一定范围内的地表位移场变化情况,计算结果表明断裂错动形成的地表垂直存在较大的空间不均匀性,且主要集中于断裂的端部即映秀、北川和青川附近,并且位移场在这些地方变化都较强烈。

objective according to 14 cases of patients with post-traumatic bronchial rupture of the ct and x-ray findings.analysis of its causes,trauma type,and ct,x-ray value and the advantages and disadvantages.methods 14 cases of bronchial rupture in patients with clinical data,x-ray,ct-chip analysis and summing up.results traumatic bronchial rupture study the performance of the main image①bronchial cut-off levy;②atelectasis and pulmonary fall levy③pleural effusion,pneumatosis;④mediastinum,subcutaneous emphysema;⑤many thoracic fractures;⑥traumatic wet lung,and so on.conclusion for traumatic bronchial rupture combined with x-ray and ct examination can be clearly diagnosed early.

目的 根据14例患者外伤后支气管断裂的ct和x线表现,分析其起因、外伤类型和ct、x线应用价值及优劣势。方法对14例支气管断裂患者的临床资料、x线平片、ct片进行分析、总结。结果外伤性支气管断裂的主要影像学表现①支气管截断征;②肺不张与肺坠落征;③胸腔积液、积气;④纵隔、皮下气肿;⑤胸廓多发骨折;⑥合并创伤性湿肺等。结论对于外伤性支气管断裂结合x线摄片和ct检查是可以早期明确诊断的。

The present configuration of the rift, which dates from the mid-Pleistocene epoch, is probably a result of a rifting process associated with thermal currents in the earth's mantle elongated depression, trough, or graben in the earth's crust, bounded on both sides by normal faults and occurring on the continents or under the oceans.

目前的断裂结构,显示来自中世纪,也许是由于断裂的过程中与热气流在地球地幔被低压延伸到地壳地堑中,位于断层的两侧正常断裂并且断裂发在陆地或者海洋。

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