西南石油大学学报(自然科学版)
西南石油大學學報(自然科學版)
서남석유대학학보(자연과학판)
JOURNAL OF SOUTHWEST PETROLEUM UNIVERSITY(SEIENCE & TECHNOLOGY EDITION)
2014年
2期
35-44
,共10页
马中远%黄苇%任丽丹%尚凯%张洁
馬中遠%黃葦%任麗丹%尚凱%張潔
마중원%황위%임려단%상개%장길
塔中%顺西地区%良里塔格组%裂缝%岩溶%油气运聚
塔中%順西地區%良裏塔格組%裂縫%巖溶%油氣運聚
탑중%순서지구%량리탑격조%렬봉%암용%유기운취
middle of Tarim Basin%Shunxi Area%Lianglitage Formation%fracture%karst effect%oil & gas migration and accumulation
塔中顺西区块位于卡塔克隆起西北倾末端,奥陶系良里塔格组储层以裂缝-溶蚀孔洞型为主。研究表明,工区内裂缝可分为构造缝和非构造缝两类,其中构造裂缝可分为垂直裂缝、斜交裂缝(高角度裂缝、低角度裂缝)和水平裂缝;非构造缝有压溶缝合线缝与成岩缝;构造裂缝中斜交裂缝相对发育,垂直裂缝和水平裂缝欠发育,斜交裂缝走向以NW、NWW向为主,次为NE走向;构造缝可大致分为3期活动,即加里东中晚期-海西早期、海西晚期和印支-燕山期。进一步分析表明,工区内构造应力场、断裂、岩性、物性和层厚与裂缝密切相关,局部构造高点、枢纽部位,转折端、断裂的交汇处、脆性岩性、物性和地层厚度等控制了裂缝的发育。工区内裂缝具有十分重要的石油地质意义,它不仅自身可作为良好的储集空间,而且是储层发生岩溶作用的有利通道并能在一定程度上扩大岩溶作用范围;在油气运聚过程中,裂缝是良好的油气运移通道,对油气成藏起着至关重要的作用。
塔中順西區塊位于卡塔剋隆起西北傾末耑,奧陶繫良裏塔格組儲層以裂縫-溶蝕孔洞型為主。研究錶明,工區內裂縫可分為構造縫和非構造縫兩類,其中構造裂縫可分為垂直裂縫、斜交裂縫(高角度裂縫、低角度裂縫)和水平裂縫;非構造縫有壓溶縫閤線縫與成巖縫;構造裂縫中斜交裂縫相對髮育,垂直裂縫和水平裂縫欠髮育,斜交裂縫走嚮以NW、NWW嚮為主,次為NE走嚮;構造縫可大緻分為3期活動,即加裏東中晚期-海西早期、海西晚期和印支-燕山期。進一步分析錶明,工區內構造應力場、斷裂、巖性、物性和層厚與裂縫密切相關,跼部構造高點、樞紐部位,轉摺耑、斷裂的交彙處、脆性巖性、物性和地層厚度等控製瞭裂縫的髮育。工區內裂縫具有十分重要的石油地質意義,它不僅自身可作為良好的儲集空間,而且是儲層髮生巖溶作用的有利通道併能在一定程度上擴大巖溶作用範圍;在油氣運聚過程中,裂縫是良好的油氣運移通道,對油氣成藏起著至關重要的作用。
탑중순서구괴위우잡탑극륭기서북경말단,오도계량리탑격조저층이렬봉-용식공동형위주。연구표명,공구내렬봉가분위구조봉화비구조봉량류,기중구조렬봉가분위수직렬봉、사교렬봉(고각도렬봉、저각도렬봉)화수평렬봉;비구조봉유압용봉합선봉여성암봉;구조렬봉중사교렬봉상대발육,수직렬봉화수평렬봉흠발육,사교렬봉주향이NW、NWW향위주,차위NE주향;구조봉가대치분위3기활동,즉가리동중만기-해서조기、해서만기화인지-연산기。진일보분석표명,공구내구조응력장、단렬、암성、물성화층후여렬봉밀절상관,국부구조고점、추뉴부위,전절단、단렬적교회처、취성암성、물성화지층후도등공제료렬봉적발육。공구내렬봉구유십분중요적석유지질의의,타불부자신가작위량호적저집공간,이차시저층발생암용작용적유리통도병능재일정정도상확대암용작용범위;재유기운취과정중,렬봉시량호적유기운이통도,대유기성장기착지관중요적작용。
Shunxi Area of middle Tarim Basin is located in the northwest pitching end of Katake uplift. Lianglitage Formation reservoir of Ordovician is mainly fracture-cavity reservoirs. The studies show that cracks can be divided into the structural ceacks and non structural cracks. The structural cracks can be divided into vertical fractures,oblique fractures(high angle fractures,low angle fractures)and horizontal fractures;the non structural cracks contain pressure dissolved stitch seam frac-tures and diagenetic fractures;the oblique fractures is relatively more than vertical fractures and horizontal fractures,and trend of oblique fractures is mainly NW,NWW,followed by NE. Structural fractures have three stages of activities:late Cale-donian-early Hercynian,late Hercynian and Indosinian-Yanshan periods. Further studies show that tectonic stress field, fracture,lithology,physical property and layer thickness is closely related to the crack. The crack growth is conteolled by local structural high,key parts,turning point,the junction of the brittle fracture,lithology,physical property and thickness of strata. Cracks in the area have very important significance in petroleum geology,which can not only be used as good reservoirs,and also favorable channel and in some extent it can expand karst effect;in the oil and gas migration and accumulation process, cracks are good oil and gas migration channel for karst effect,plays a vital role in oil and gas accumulation.