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fault block

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fault block 【地質學；地理學】(兩個斷層間的)零亂巖石。

【地質學；地理學】(兩個斷層間的)零亂巖石。 “fault“ 中文翻譯：   n. 1.過失，過錯；罪過，責任。 2.缺點，缺陷，瑕疵 ...“block“ 中文翻譯：   n. 1.片，塊，大塊；粗料，毛料；木料；石料；金屬塊； ...“block fault“ 中文翻譯：   地塊斷層; 塊斷層“block-fault“ 中文翻譯：   塊斷層“antithetic block fault“ 中文翻譯：   對偶塊狀斷層“block fault pattern“ 中文翻譯：   塊狀斷裂模式; 塊狀斷裂型“block-fault structure“ 中文翻譯：   塊狀斷裂構造“detached fault block“ 中文翻譯：   擠離斷塊“fault block basin“ 中文翻譯：   斷塊盆地“fault block mountain“ 中文翻譯：   斷塊山“fault block oil reservoir“ 中文翻譯：   斷塊油藏“fault block pool“ 中文翻譯：   斷塊油氣藏“fault block reservoirs“ 中文翻譯：   斷塊油氣藏“fault block tectonism“ 中文翻譯：   塊斷構造酌“fault block terrain“ 中文翻譯：   斷塊地帶“fault-block architecture“ 中文翻譯：   斷塊構造“fault-block basin“ 中文翻譯：   斷塊盆地“fault-block closure“ 中文翻譯：   斷塊閉合構造“fault-block gas reservoir“ 中文翻譯：   斷塊氣藏“fault-block mountain“ 中文翻譯：   斷塊山“fault-block mountains“ 中文翻譯：   斷塊山“fault-block movement“ 中文翻譯：   斷塊運動“fault-block structure“ 中文翻譯：   斷塊構造“fault-block topography“ 中文翻譯：   斷塊地形“fault-block valley“ 中文翻譯：   斷塊谷

faultage

Based on the geological , hydrogeological and hydrochemical information , the genesis of the underground hot water in qi county of shanxi has been analyzed . it is concluded that the formation of underground hot water is related to the magmatic activity in yanshan period , the goup of the base fault block forming in new tectonic period , the large depth and fast variety to underground water cycle 從地質、水文地質、水化學等方面，分析了祁縣地區地下熱水成因，得出該地區地下熱水形成與燕山期巖漿活動、新構造運動形成的基底斷塊隆起及地下水循環深度大、交替迅速有關。

The production of no57 & 67 fault block in xinzhuang oil - field is taken as an example to analyse the developing complexity and difficultly , which concludes the producing characteristics , effect factors of normal production and flooded well , meanwhile , a simple method is put forwared to judge the water invasion based on the conclusion of various kinds of producing wells 作者以新莊油田57和67斷塊稠油開發為例，通過分析判斷，分別研究了層間水侵入井和正常生產井的開發特點及影響因素，提出見層間水的判斷方法。

Depositional cycles on basin scale have been interpreted as the result of depositional response to tectonism such as episodic rifting , polyphasic compressive flexural subsidence and reversion , and differential subsidence of fault blocks ; while the formation of high frequency sequences was attributed to variation in lake level and sediment supply 盆地規模的沉積旋回多是盆地幕式裂陷、多幕擠壓撓曲沉降、多期構造反轉、斷塊差異沉降等構造作用的沉積回應；高頻層序單元的發育則主要與湖平面和沉積物供給量的變化有關。

According to the theory of developing viscous crude with screw pump and combined with the reservoir characteristic and oil property , fault block 70 is developed reasonably and effectively through a series of corollary technique including chemical pre - processing in the formation , viscosity decrease in the well bore , down - hole anchoring of screw pump , optimized design of screw pump , reasonable determination of the turning rate of screw pump , frequency alternating control , heat exchange and viscosity decrease in well head , monitoring of screw pump 依據螺桿泵開采重油的理論，結合澤70斷塊稠油油藏的特點和原油物性，通過實施地層化學預處理、井筒降粘、螺桿泵井下錨定、螺桿泵優化設計、螺桿泵合理轉速的確定、變頻控制、井口換熱降粘、螺桿泵監測等一系列螺桿泵配套工藝技術，使澤70斷塊得以合理有效的開發。

Zhuangxi hill is the typical example of fold hill and chegu201 hill is typical in fault block hills . we analyze them detailedly , set up the geology models of forming process , and analyze the relationship of forming process and petroleum and gas migration , and describe their character of reservoir , we do simulation experiment for the formation procession of zhuangxi hill 對各類潛山的典型實例廣饒潛山、樁西潛山和車古201潛山進行了具體的分析，建立了潛山形成過程地質模型，分析了其與油氣成藏的關系，描述了成藏特征。

Based on these , this paper studied deeply the main factors controlling accumulation and distribution of oil or gas and accumution models through studying types of oil or gas reservoirs and oil or gas distribution laws of f , y oil layers in the north of songliao basin . this paper pointed out sourcerocks , caprocks , faults and hydrodynamics power to be the main factors controlling oil or gas accumulation and distribution . there are - two models of oil or gas accumulating in fault - lithology or fault block traps through migrating downward under the regional caprock and oil or gas from sourcerock downward accumulating in fault - lithology or fault block traps in reservoirs upward by migrating through fau lts 在此基礎上，通過對松遼盆地北部扶、楊油層油氣藏類型及分布規律分析，深入研究了扶、楊油層油氣成藏與分布的主控因素和成藏模式，指出源巖、蓋層、斷裂和水動力是松遼盆地北部扶、楊油層油氣成藏與分布的主控因素，具有被下油氣倒灌運移于斷層?巖性或斷塊圈閉成藏和下生上儲天然氣沿斷裂運移斷層?巖性或斷塊圈閉成藏二種模式。

The obvious effects have been made in the adjustment of injection to - producing and water blocking by applying comprehensively the log information of degree of saturation and profile - log and tracer survey information to tap the zone of enrichment of remaining oil potential , analyze the direction of injected water streamline and guide the measures for tapping potential in tuo 7 fault block 摘要總結了坨七斷塊綜合應用飽和度測井資料、吸水剖面資料、水井注示蹤劑資料，發掘剩余油潛力富集帶、分析注水流線方向，指導油井措施挖潛、注采調整和堵水調剖工作所取得的明顯效果。

Rb - sr whole rock - minerals ages determination indicates that the isochronal ages are 25018 ma and 213 . 09 . 8 ma for suhaitu and wenduerhao intrusion , respectively . the dated isotopic ages demonstrate that the alxa alkaline - rich intrusive rocks belong to indosinian alkaline magma activity . the similarities and differences of the alkaline - rich intrusive rocks distributed in the alxa fault block and those distributed along the northern margin of the north china block and the tarim block are compared and discussed 采用rb - sr法對阿拉善斷塊有代表性的蘇亥圖溫都爾浩富堿侵入巖體的年進行了測定，分別獲得25018 ma和213 . 09 . 8 ma的年值，提供了屬于印支期的年代學證據，認為阿拉善斷塊北緣富堿侵入巖和華北斷塊北緣燕遼陰山印支期富堿性侵入巖帶應該劃歸同一印支期富堿性侵入巖帶。

Fourthly , summarized the methods and the principals for pre - stack and post - stack 4 - d seismic data processing ; proposed the criteria for seismic data process ; built a set of processing flow . through the real data processing ( 029 fault block ) , obtained reasonable results . the processed result was approved by the further production well 第四，總結了迭前、迭后四維地震資料處理的方法與原理，針對高29斷塊的實際資料，提出了處理準則，建立了處理流程，獲得了良好的處理效果，并得到開發開發調整井的證實。

This paper presents the prestack time migration to curved rays for minor fault blocks , which is of more accurate migration , allowing the travel - time equation to be more close to the real pathway of layered media seismic wave propagation , the focused imaging to be more precise , the migrated results to be of good preserved amplitude processing property and the output trace gathers to be used for the lithologic analysis and inversion study 采用彎曲射線疊前時間偏移技術使小斷塊準確偏移歸位，其走時方程更接近層狀介質地震波的真實傳播路徑，成像聚焦更精確，且通過特殊振幅處理，其偏移結果有很好的保幅性，輸出的道集可以用于巖性分析和反演研究。

Through research , the organic matter of source rocks in carboniferous - permian coal measure strata began first hydrocarbon - generating in mesozoic , and the first hydrocarbon - filling took place . but , because of yanshan movement later , the carboniferous - permian strata rose , as a result , the first hydrocarbon - generating and reservoir - forming paused ; in early tertiary period , because carboniferous - permian strata dipping forward east originally turned into dipping forward west , the prototype of faulted block began to form gradually ; by the end of sha - 3 period of early tertiary , the paleogeotherm of carboniferous - permian strata exceed the mesozoic ' s temperature again , and accordingly , abundant hydrocarbon was generated and expulsed secondly . the trap continued to develop ; from the end of late tertiary to quaternary , the second hydrocarbon - generating and expulsing got to its peak , and the second reservoir - forming was over 研究表明，本區石炭?二疊紀烴源巖在中生代發生一次生烴和排烴，并有油氣充注，后因燕山運動導致地層抬升，一次生烴和成藏過程中止；在早第三紀，原來東傾的地層變為西傾，斷塊圈閉開始具雛形；至早第三紀沙二末期，石炭?二疊系的大部分地層古地溫再次超過中生代一次生烴的溫度，開始二次生烴和排烴，圈閉持續發育；晚第三紀末?第四紀，二次生烴、排烴達到高峰，二次成藏完成。

The frontal structure of longmenshan in the west of sichuan is very complex , showing intense structure deformation in overthrust belt , high structure amplitude , steep stratigraphic dip , developed fault blocks , complex seismic wave field , frequent change of lateral velocity , and poor image of post - stack time migration processing 摘要川西龍門山前緣構造非常復雜，逆掩推覆構造帶構造形變強烈，構造幅度大，地層傾角陡，斷塊發育，地震波場復雜，速度橫向變化大，常規疊后時間偏移處理成像效果較差。

On the basis of enough sources , better relations of space arrangement of oil generation , migration and reserver , good conditions of reservoirs and caprocks , subtle reservoirs are formed , such as lithological reservoirs , stratigraphic overlapping reservoirs , fault block reservoirs , palaeoburied reservoirs and fault - nose reservoirs 在油源充足，良好的生運儲空間配置關系，優越的儲層條件和蓋層條件的基礎上，形成了巖性油氣藏、地層超覆油氣藏、斷塊油氣藏、古潛山油氣藏和斷鼻構造油氣藏等多種類型的隱蔽油氣藏。

The slope zone in northern biyang sag is characterized by complex structure , developed minor fault blocks , varied seismic vertical and horizontal velocities and difficult to get imaging , which result in that conventional imaging approaches are hard to meet the needs for exploration and development of this area 摘要泌陽凹陷北部斜坡帶構造復雜，小斷塊發育，地震縱、橫向速度變化劇烈，成像困難，常規的地震成像方法成果難以滿足勘探開發的需要。

In addition , side - tracking in old wells can produce residual oil between wells and on structural high , improve pattern arrangement , and control bottom water coning ; it is an effective method for developing minor fault block reservoir with complex lithology and bottom water 同時，老井側鉆既能挖掘井間及高部位剩余油，完善井網，又能有效控制底水錐進，是復雜底水小斷塊油藏經濟高效開發的措施方法。

Based on a vast amount of literature study on 4 - d seismic and the investigation of petrophysical properties in buohai bay areas , the author implemented a pilot research about 4 - d seismic in a water driven reservoir in gao29 fault block 本文在大量文獻調研的基礎上，以渤海灣地區巖石物理參數研究為基礎，結合高29斷塊兩次采集的三維地震資料全面、系統地開展了水驅四維地震先導試驗研究。

Effected by many factors during huff and puff , the reservoir of edge water invasion and complex small fault block , the producing wells which are located in the neighborhood of the fault trace and oil - water contact , are quite difficult for development 摘要由于在蒸汽吞吐開發過程中要受到多種因素的影響，而且生產井處于斷層和油水邊界附近，所以層間水復雜小斷塊稠油油藏的開發難度較大。

5 ) the best exploration area of reservoir prospecting is the region locating on the north of well - huo no . 14 block . by the accurate structural interpreting we have found a trap deploymented a exploratory well hi it - - - - - - north fault block of well - huono . 14 儲層預測的有利勘探區? ?火14井北面區域，通過構造精細解釋已發現火14井北斷塊圈閉，并部署一口預探井。

They are dimorphism hill trap > fold hill trap and fault block hill trap . we mark off the hill kinds in term of the cause of hill formation in this research . they are dimorphism hilk fold hill and fault block hill 總結山五種不同類型的潛山帶，在這五種不同類型的潛山帶上按其成因，主要分為三種類型的圈閉?風化殘丘山圈閉、拱張褶皺山圈閉利斷裂塊斷山圈閉。