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)
2013年
1期
43-51
,共9页
马中良%郑伦举%李志明%秦建中
馬中良%鄭倫舉%李誌明%秦建中
마중량%정륜거%리지명%진건중
盐类%烃源岩%热压模拟实验%油气生成%非常规油气资源
鹽類%烴源巖%熱壓模擬實驗%油氣生成%非常規油氣資源
염류%경원암%열압모의실험%유기생성%비상규유기자원
salt%source rock%thermocompression simulation experiment%hydrocarbon generation%unconventional oil and gas resources
根据中国东部下第三系盐湖相沉积存在的地质实际,利用地层孔隙热压生排烃模拟仪开展了仿真地层条件下的含盐和不含盐泥质烃源岩的生排烃模拟实验,通过对烃类产物的分析探讨了盐类物质参与烃源岩生排烃的过程.研究表明:(1)盐类的存在加速了成烃演化,促进了石油和天然气的生成;(2)盐类的存在降低了对有机质的吸附能力,加速了粘土转化和脱水过程,且盐层易解理,使烃源岩中微孔隙及孔缝发育,促进了油气的初次运移;(3)无盐泥质源岩发育区虽然滞留大量的石油资源,但由于其岩石本身难压裂,对于商业化开采页岩油并无太大意义,到达过成熟阶段后,可能是页岩气开采的有利区带.盐岩发育区虽然其整体演化过程中生成的油气易于排出,但在Ro=1.28%时仍然滞留着20%的石油资源,富含大量的盐类脆性矿物而低含粘土矿物,有利于产生裂缝,易于压裂,是页岩油藏勘探的有利区带.
根據中國東部下第三繫鹽湖相沉積存在的地質實際,利用地層孔隙熱壓生排烴模擬儀開展瞭倣真地層條件下的含鹽和不含鹽泥質烴源巖的生排烴模擬實驗,通過對烴類產物的分析探討瞭鹽類物質參與烴源巖生排烴的過程.研究錶明:(1)鹽類的存在加速瞭成烴縯化,促進瞭石油和天然氣的生成;(2)鹽類的存在降低瞭對有機質的吸附能力,加速瞭粘土轉化和脫水過程,且鹽層易解理,使烴源巖中微孔隙及孔縫髮育,促進瞭油氣的初次運移;(3)無鹽泥質源巖髮育區雖然滯留大量的石油資源,但由于其巖石本身難壓裂,對于商業化開採頁巖油併無太大意義,到達過成熟階段後,可能是頁巖氣開採的有利區帶.鹽巖髮育區雖然其整體縯化過程中生成的油氣易于排齣,但在Ro=1.28%時仍然滯留著20%的石油資源,富含大量的鹽類脆性礦物而低含粘土礦物,有利于產生裂縫,易于壓裂,是頁巖油藏勘探的有利區帶.
근거중국동부하제삼계염호상침적존재적지질실제,이용지층공극열압생배경모의의개전료방진지층조건하적함염화불함염니질경원암적생배경모의실험,통과대경류산물적분석탐토료염류물질삼여경원암생배경적과정.연구표명:(1)염류적존재가속료성경연화,촉진료석유화천연기적생성;(2)염류적존재강저료대유궤질적흡부능력,가속료점토전화화탈수과정,차염층역해리,사경원암중미공극급공봉발육,촉진료유기적초차운이;(3)무염니질원암발육구수연체류대량적석유자원,단유우기암석본신난압렬,대우상업화개채혈암유병무태대의의,도체과성숙계단후,가능시혈암기개채적유리구대.염암발육구수연기정체연화과정중생성적유기역우배출,단재Ro=1.28%시잉연체류착20%적석유자원,부함대량적염류취성광물이저함점토광물,유리우산생렬봉,역우압렬,시혈암유장감탐적유리구대.
According to the presence of aalt lake sediments of the Tertiary in the east of China,we make use of hydrocarbon generation and expulsion of pore hot simulation instrument to carry out the simulation under the conditions of formation of salt and no salt argillaceous source rock hydrocarbon generation and expulsion simulation experiments,through the analysis of hydrocarbon products of the salts in hydrocarbon source rocks in the process of hydrocarbon generation and expulsion. The results have shown that:(1)the presence of salts accelerated the evolution of hydrocarbon generation,and promoted oil and gas generation.(2)the presence of salt reduces the adsorption capacity of organic matter,accelerated the process of transformation and dehydration of clay,and promoted the initial operation of oil and gas shift easy cleavage and other reasons,the source rocks in the development of micro-pores and apertures in source rocks.(3)Although there exist a large number of stranded oil resources,salt-free zones in shale source rocks has little value of commercial exploitation because of the difficulties in fracturing. But they may be favorable of shale rock gas exploitation when reaching maturing. Although it is easy to discharge oil and gas generated in the process of evolution of salt rocks,20%of oil resources were still stuck,when Ro=1.28%a large number of salts rich in minerals and low brittleness with clay minerals,are conducive to creating cracks,and are easy for fracturing,which makes salt rock areas favorable shale zones for reservoir exploration.