油气藏评价与开发
油氣藏評價與開髮
유기장평개여개발
2012年
5期
1-5
,共5页
王彭%梁则亮%朱雨萍%邓先伟%杨扬
王彭%樑則亮%硃雨萍%鄧先偉%楊颺
왕팽%량칙량%주우평%산선위%양양
中拐凸起%石炭系%火山岩%裂缝预测
中枴凸起%石炭繫%火山巖%裂縫預測
중괴철기%석탄계%화산암%렬봉예측
Zhongguai uplift%development degree%carboniferous%fractures prediction
裂缝是形成火山岩有效储层的必要条件。从中拐凸起现今构造形迹特征入手,利用有限元数值分析技术,模拟工区石炭系火山岩储层的古构造应力场和破裂接近程度系数(η);将η与实际资料和野外观测结果对比,确定不同裂缝发育级别及其对应的η值;结合构造地质学理论以及生产实际,对中拐凸起石炭系火山岩储层裂缝的发育程度、裂缝类型及产状进行预测。预测结果表明:中拐凸起石炭系火山岩裂缝非常发育,裂缝分布比较有规律性,主要分布在沿北东向的克-乌断裂带、南北向的红车断裂带及红3井东断裂两侧,裂缝主要发育方位为东西向(EW)、北东向(NE)和北北西(NNW),裂缝的主要类型为高角度剪切缝。
裂縫是形成火山巖有效儲層的必要條件。從中枴凸起現今構造形跡特徵入手,利用有限元數值分析技術,模擬工區石炭繫火山巖儲層的古構造應力場和破裂接近程度繫數(η);將η與實際資料和野外觀測結果對比,確定不同裂縫髮育級彆及其對應的η值;結閤構造地質學理論以及生產實際,對中枴凸起石炭繫火山巖儲層裂縫的髮育程度、裂縫類型及產狀進行預測。預測結果錶明:中枴凸起石炭繫火山巖裂縫非常髮育,裂縫分佈比較有規律性,主要分佈在沿北東嚮的剋-烏斷裂帶、南北嚮的紅車斷裂帶及紅3井東斷裂兩側,裂縫主要髮育方位為東西嚮(EW)、北東嚮(NE)和北北西(NNW),裂縫的主要類型為高角度剪切縫。
렬봉시형성화산암유효저층적필요조건。종중괴철기현금구조형적특정입수,이용유한원수치분석기술,모의공구석탄계화산암저층적고구조응력장화파렬접근정도계수(η);장η여실제자료화야외관측결과대비,학정불동렬봉발육급별급기대응적η치;결합구조지질학이론이급생산실제,대중괴철기석탄계화산암저층렬봉적발육정도、렬봉류형급산상진행예측。예측결과표명:중괴철기석탄계화산암렬봉비상발육,렬봉분포비교유규률성,주요분포재연북동향적극-오단렬대、남북향적홍차단렬대급홍3정동단렬량측,렬봉주요발육방위위동서향(EW)、북동향(NE)화북북서(NNW),렬봉적주요류형위고각도전절봉。
Fracture is a necessary condition for volcanic effective reservoir. Starting by studying on the present structural features of Zhongguai uplift, finite element numerical analysis technique was used to imitate the paleotectonic stress field and fracturing prox-imity coefficientηof fractures of the carboniferous volcanic reservoir. Fracture development degree and the correspondingηvalues were determined through correlation of η with real data and field observation. The development degree, types and occurrence of fractures were comprehensively predicted by using these criteria and in combination with theories of structural geology and actual production condition. The results showed that fractures were well developed in the carboniferous volcanic reservoir of Zhongguai up-lift. The distribution of fractures was relatively regular, which mainly distributed along the N-E Ke-Wu fault zones, N-S Hongche fault zones and both sides of Hong-3 well eastern fault. The mainly development azimuths of fracture were E-W, N-E and N-N-W. The principal types of fractures were dominated by high angle shear fractures.