石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2013年
6期
683-688
,共6页
原油%烃源岩%油源对比%油气藏%巴楚-麦盖提地区%塔里木盆地
原油%烴源巖%油源對比%油氣藏%巴楚-麥蓋提地區%塔裏木盆地
원유%경원암%유원대비%유기장%파초-맥개제지구%탑리목분지
crude oil%source rock%oil/source correlation%oil and gas pool%Bachu-Maigaiti area%Tarim Basin
巴楚-麦盖提地区是重要的油气聚集区。玉北地区玉北1井在奥陶系鹰山组测试获25.2 m3/d的海相工业油气流。玉北奥陶系油藏与巴什托(普)油气田的原油是否同源是困扰该地区油气勘探并急需解决的问题之一。通过玉北1井、巴什托(普)主要油气藏(田)的原油地球化学特征研究、油-油对比、油源对比等综合分析,并类比塔河奥陶系原油进行了巴楚-麦盖提地区主要油气藏原油地球化学特征及油源探讨分析。综合研究认为玉北地区奥陶系的原油地球化学特征与塔河奥陶系原油相近。通过烃源有机相类比,认为玉北地区奥陶系原油可能来自塔西南地区中下寒武统斜坡相烃源岩;巴什托轻质油推测主要来自盆地-陆棚相寒武系烃源岩,部分来源于海陆交互相石炭系。
巴楚-麥蓋提地區是重要的油氣聚集區。玉北地區玉北1井在奧陶繫鷹山組測試穫25.2 m3/d的海相工業油氣流。玉北奧陶繫油藏與巴什託(普)油氣田的原油是否同源是睏擾該地區油氣勘探併急需解決的問題之一。通過玉北1井、巴什託(普)主要油氣藏(田)的原油地毬化學特徵研究、油-油對比、油源對比等綜閤分析,併類比塔河奧陶繫原油進行瞭巴楚-麥蓋提地區主要油氣藏原油地毬化學特徵及油源探討分析。綜閤研究認為玉北地區奧陶繫的原油地毬化學特徵與塔河奧陶繫原油相近。通過烴源有機相類比,認為玉北地區奧陶繫原油可能來自塔西南地區中下寒武統斜坡相烴源巖;巴什託輕質油推測主要來自盆地-陸棚相寒武繫烴源巖,部分來源于海陸交互相石炭繫。
파초-맥개제지구시중요적유기취집구。옥북지구옥북1정재오도계응산조측시획25.2 m3/d적해상공업유기류。옥북오도계유장여파십탁(보)유기전적원유시부동원시곤우해지구유기감탐병급수해결적문제지일。통과옥북1정、파십탁(보)주요유기장(전)적원유지구화학특정연구、유-유대비、유원대비등종합분석,병류비탑하오도계원유진행료파초-맥개제지구주요유기장원유지구화학특정급유원탐토분석。종합연구인위옥북지구오도계적원유지구화학특정여탑하오도계원유상근。통과경원유궤상류비,인위옥북지구오도계원유가능래자탑서남지구중하한무통사파상경원암;파십탁경질유추측주요래자분지-륙붕상한무계경원암,부분래원우해륙교호상석탄계。
Bachu-Maigaiti area is an important focus area of oil and gas. In the Ordovician Yingshan Formation in well Yubei 1, industrial oil and gas flows of marine facies have been tested for 25.2 m3/d. It is urgent to solve the problem whether the crude oils from Ordovician of Yubei area and Bashituo oil field are of the same sources. Through the geochemical analysis, oil/oil and oil/source correlations of the crude oils from well Yubei 1 and Bashituo oil field, compared with the Ordovician crude oils from Tahe area, the geochemical characteristics of crude oil and oil source of the main oil-and-gas reservoirs in Bachu-Maigaiti area are discussed. The geochemical features of the Ordovician crude oils from Yubei area are similar to those of the Ordovician crude oils from Tahe area. According to the organic analogy of oil source, the Ordovician crude oils from Yubei area may originate from the Middle and Lower Ordovician source rocks of slope facies in the southwestern Tahe area. The light oils from Bashituo area mainly come from the Cambrian source rocks of basin-shelf facies, and partially from the Car-boniferous source rocks of marine-terrigenous facies.