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
認為壩縣束鹿邯鄲斷裂帶、唐山河間磁縣斷裂帶和黃驊德州東明斷裂帶3條
北東向右旋走滑斷裂帶為華
北平原裂谷系從早第三紀伸展拉張作用進入晚第三紀第四紀走滑剪切拉張作用的產物，這3條斷裂帶分別位於3個
北東向
坳陷帶中部，並構成了第四紀沉降中心，與營口濰坊斷裂帶起構成華
北平原內的主要強震構造。
Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin
通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和
坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地
北部朝陽溝?駱駝營子地熱勘查遠景區。
Jiyang depression is a field where nonhydrocarbon is rich. these resources have close relation with the activities of the volcanos. at the same time, the activities of volcanos have deep contact with the activities of the faults. the growth of the faults in jiyang depression is great. by the research of the index number of the faults growth and the other researches, nw direction faults are the most ones in mesozoic, nw and ne and approximately ew directions all exist in cenozoic. the above reflects the whole geotectonic background that sinistral shearing stress field exists in mesozoic, but dextral shearing stress field exists in cenozoic
這些氣藏與火山活動有密切的成生關系，同時火山活動與斷裂活動也有密切的關系。濟陽
坳陷內斷裂活動極為發育，通過斷層生長指數等的分析，推斷中生代斷裂以
北西向為主，新生代則兼有
北西向
北東向和近東西向的斷裂，上述斷裂發育特徵反映了該區的大地構造背景，在中生代是左旋的剪切應力場，在新生代則是右旋的剪切應力場。
It rested in the lap of an undulating upland adjoining the north wessex downs.
它坐落在和
北維塞司的丘陵相連那片起伏高原中間一個山
坳里。
Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences. the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )
通過研究有以下成果及認識：鄂爾多斯盆地及其周緣地區沉積蓋層可劃分為五大構造層序，盆地的形成和演化分為六大構造階段：太古代至古元古代基底形成階段、中新元古代克拉通內裂陷槽或
坳拉槽演化階段、震旦紀?早古生代華
北陸表海盆演化階段、晚古生代?早中生代華
北克拉通
坳陷演化階段、中生代中晚期大鄂爾多斯內陸盆地演化階段及獨立鄂爾多斯盆地的形成、新生代周緣斷陷盆地演化階段。
The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep. under the background of indian plate subducting under asia - europe plate, bachu forebulge was greatly affected by the development of southwest depression and awati depression. almost all of its structure reversed, and as a result of it, both of its south and north boundary migrated. according to its evolution history and its feature, the authors tentatively use both - side migration model to interpret the evolution of compound forebulge. since triassic, almost all the spheres above lithosphere synchronously became flexure. because transpressional stress field became increasingly strong, bachu forebulge continued uplifting and big faults formed. then, bachu uplift, as a whole, slipped upward along those big faults and showed migrating toward thrust zone in plane. in tectonic tranquility, the lithosphere bounded back and in consequence of it, bachu uplift slipped down and showed migration toward craton, at that moment negative inversion structures developed. while the forebulge migrated toward its south and north foredeep, it was very possible that locally extensional stress appeared in the forebulge
在印度板塊向歐亞板塊俯沖的大背景下，巴楚前緣斷隆受西南
坳陷和阿瓦提凹陷的影響，新生代時構造體制發生反轉，邊界向南
北遷移。根據其發育過程特徵，作者用復合前緣隆起兩端遷移模式對復合前緣隆起獨特的構造發育史進行了解釋：即三疊紀以來巖石圈各圈層同步撓曲變形。隨著擠壓應力場的增大，巴楚隆起在撓曲基礎上不斷抬升，形成幾條大型斷裂帶。
According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin
依據理論分析及勘探實踐，優選出4個有利的勘探區帶，它們是：庫車前陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉；準南前陸沖斷帶第二、第三排構造帶；川西
北部及南部燕山運動期古隆起、川中平緩褶皺構造帶以及深
坳陷內部的非常規天然氣；柴
北緣冷湖南八仙構造帶。
Jiyang depression ; faults ; growth index number ; nw ; ne ; approximately ew
濟陽
坳陷斷裂生長指數
北西向
北東向近東西向
Being primarily controlled by northwest faults, cretaceous of jiyang depression contained several isolated basins, and lake levels of these isolated basins were instable, but on the whole, shore and shallow lake sub - facies is in the majority
北西向斷層的活動對沉積起到主要的控製作用，在其控制下，白堊紀濟陽
坳陷為一相互分割的山間盆地，湖盆范圍時大時小，湖水深度不斷變化，總體湖水較淺，主要發育濱淺湖亞相。
With an area of 5300 km2, dongpu depression is located in the southwest of lin - qing depression, bohaiwan basin, bounded with lu - xi uplift by lan - liao fault in the east, with nei - huang uplift by chang - yuan fault in the west, with lan - kao heave by the north feng - qiu fault in the south, with xin country depression by ma - ling fault in the north, while spreading along nne defection, taking on the forms of being wide in the south, and narrow in the north. it is a rift fault depression basin with the characteristics of striking, with the basement being the paleozoic and mesozoic, and the capping beds being the cenozoic
東濮凹陷位於渤海灣盆地臨清
坳陷西南端，東側以蘭聊斷裂為界與魯西隆起為鄰，西側以長垣斷裂為界與內黃隆起相接，南以封丘
北斷層為界與與蘭考凸起相鄰，
北以馬陵斷層為界與與莘縣凹陷相望，是以古?中生界為基底，以新生界為蓋層，古近紀形成的拉分走滑?裂谷型箕狀斷陷盆地。
Again, i do not recommend that you take the risk to get to the scene. make do with the annual report and enjoy a safe hike to ham tin, where you should get off the trail, go on to the beach, cross the shaky bridge at the end, have a good lunch and refill at the restaurant run by my old friend mr lai
我們繼續走到咸田，然後離開麥理浩徑，到達沙灘，經過沙灘盡頭那道搖搖晃晃的獨木橋，在我的老友黎先生的士多吃頓午餐，休息一下，然後再踏上士多後面的路回到麥理浩徑上，一直前往大浪
坳赤徑及
北潭凹。
The very experienced and fit hikers can instead go over to the far end of tai wan where they can take on the challenging sharp peak before returning via nam she au and tai long au, etc. remember to bring along a copy of the 2002 hkma annual report
當然，經驗豐富體能又好的遠足朋友則可以從咸田盡頭，跨過小山，去到大灣，再從大灣的盡頭，走上險要的蚺蛇尖，然後才經蚺蛇
坳及大浪
坳等返回
北潭涌。
Cenozoic sequence stratigraphy and characteristics of the sedimentary system in the shubei area, liaohe basin
遼河
坳陷曙
北地區新生代層序地層及沉積體系發育特徵
Ft. of residential land. those villages that were affected included lee uk, chow uk, man uk, sha tsui, lan lai wan, ko tong, ha yeung, uk tau village, pak tam chung and pak tam au. roughly speaking, there were about 50 families living in these villages. about 300 to 400 people were resettled in sai kung town, where blocks of 5 - storey houses were built for this purpose. approximately 20 to 30 families of boat people affected, however, were resettled on land
1萬平方尺建築地，直接受影響的村落分別有李屋、周屋、萬屋、沙咀、爛泥灣等，估計居民約有50餘戶，人口至少有400 ，其中的300至400名居民被遷往西貢墟新建五層樓宇，被遷移上岸的水上人家約有20至30戶，其他受波及的村落包括高塘、下洋、屋頭村、
北潭涌、
北潭
坳等地。
With a differential accumulation analysis of the fault closeness and the difference of faulted reservoir in beitang depression, it is suggested that ( 1 ) an inactive fault in clastic sequence may mainly restrict hydrocarbon migration ; ( 2 ) undercompacted shales with overpressure can lead to strongly restricting hydrocarbon migration along faults ; ( 3 ) hydrocarbon segregation associated with fault traps more probably takes place in undercompacted zone with abnormal hydropressure
通過黃驊
坳陷
北塘凹陷斷層的封閉性及斷層油氣藏差異聚集分析，表明斷層在活動停止期主要起封閉作用，但在正常壓實層序段仍有少量輕組分的烴類沿斷層發生運移而引起差異聚集；而在欠壓實帶，異常高孔隙流體壓力使斷層在縱向上具有很強的封閉性。
Reservoir characteristics of dongying formation in the middle - north area of huanghua depression
黃驊
坳陷中
北區東營組儲層特徵研究
At the same time, attained following fruits : 1. the tectonic analysis indicated that the distortion of the foreland basin was mainly attributed to the movements of longmen mountains, the structural features, forming periods, and transformation fashions are different between the northern and southern segments
主要取得如下成果： 1 、構造研究表明川西
坳陷形成與形變主要受控于龍門山造山帶，表現為
坳陷內部南、
北段構造特徵、形成期及其變形方式上的差異。
Chengdao oil field is a big anticine structure which developed basing on pretertiary sub - mountain. it surrounded by bozhong depression and chengbei sag with good reservoir - forming condition
埕島油田是在前第三系潛山背景上發育起來的大型披覆構造，東連渤中坳陷，西南接埕北凹陷，有著良好的油氣成藏條件。
