地质科技情报
地質科技情報
지질과기정보
GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION
2010年
2期
95-99
,共5页
陈玲%马昌前%凌文黎%佘振兵%陈子万
陳玲%馬昌前%凌文黎%佘振兵%陳子萬
진령%마창전%릉문려%사진병%진자만
麻江古油藏%油气成藏年代学%沥青%Re-Os同位素%热电离质谱
痳江古油藏%油氣成藏年代學%瀝青%Re-Os同位素%熱電離質譜
마강고유장%유기성장년대학%력청%Re-Os동위소%열전리질보
Majiang paleo-oil pool%geochronology of hydrocarbon accumulation%bitumen%Re-Os isotope%thermal ionization mass spectrometry
利用Re-Os同位素方法开展富含有机质的沥青、原油等的研究,是确定油气成藏时间和破坏时间有效的但极富挑战性的新途径,在国内尚无研究实例报道.以我国南方最大的古油藏之一的麻江古油藏中的沥青为主要对象,采用Re-Os同位素方法试图限定油气的成藏时间和破坏时间.研究表明,麻江古油藏的固体沥青Re、Os同位素质量分数分别在41.5×10~(-6)~642×10~(-6)和0.21×10~(-6)~12.15×10~(-6)之间,N(~(187)Re)/N(~(188)Os)比值较高,且变化范围较大,在270.90~4 074.99之间,Os同位素组成指示中等放射成因,其N(~(187)Os)/N(~(188)Os)比值在0.340 0~3.655 7之间变化.所有沥青样品的模式年龄在28~144 Ma之间变化,集中在85 Ma左右.通过沥青Re-Os同位素研究,结合详细地质资料,认为麻江古油藏的成藏时间为印支期-早燕山期(144 Ma之前),而油藏破坏时间为燕山晚期即85 Ma左右.
利用Re-Os同位素方法開展富含有機質的瀝青、原油等的研究,是確定油氣成藏時間和破壞時間有效的但極富挑戰性的新途徑,在國內尚無研究實例報道.以我國南方最大的古油藏之一的痳江古油藏中的瀝青為主要對象,採用Re-Os同位素方法試圖限定油氣的成藏時間和破壞時間.研究錶明,痳江古油藏的固體瀝青Re、Os同位素質量分數分彆在41.5×10~(-6)~642×10~(-6)和0.21×10~(-6)~12.15×10~(-6)之間,N(~(187)Re)/N(~(188)Os)比值較高,且變化範圍較大,在270.90~4 074.99之間,Os同位素組成指示中等放射成因,其N(~(187)Os)/N(~(188)Os)比值在0.340 0~3.655 7之間變化.所有瀝青樣品的模式年齡在28~144 Ma之間變化,集中在85 Ma左右.通過瀝青Re-Os同位素研究,結閤詳細地質資料,認為痳江古油藏的成藏時間為印支期-早燕山期(144 Ma之前),而油藏破壞時間為燕山晚期即85 Ma左右.
이용Re-Os동위소방법개전부함유궤질적력청、원유등적연구,시학정유기성장시간화파배시간유효적단겁부도전성적신도경,재국내상무연구실례보도.이아국남방최대적고유장지일적마강고유장중적력청위주요대상,채용Re-Os동위소방법시도한정유기적성장시간화파배시간.연구표명,마강고유장적고체력청Re、Os동위소질량분수분별재41.5×10~(-6)~642×10~(-6)화0.21×10~(-6)~12.15×10~(-6)지간,N(~(187)Re)/N(~(188)Os)비치교고,차변화범위교대,재270.90~4 074.99지간,Os동위소조성지시중등방사성인,기N(~(187)Os)/N(~(188)Os)비치재0.340 0~3.655 7지간변화.소유력청양품적모식년령재28~144 Ma지간변화,집중재85 Ma좌우.통과력청Re-Os동위소연구,결합상세지질자료,인위마강고유장적성장시간위인지기-조연산기(144 Ma지전),이유장파배시간위연산만기즉85 Ma좌우.
Rhenium-Osmium isotope system is a new and challenging method used to determined the hydrocarbon accumulation and date of desdtruction. This paper reports a Re-Os approach to date the hydrocarbon accumulation and destruction time of the Majiang paleo-oil pool, one of the largest paleo-oil reservoirs in South China. The Re and Os contents in the bitumen vary from 41.5×10~(-6) to 642×10~(-6) and 0.21×10~(-6) to 12.15×10~(-6), respectively. Their ~(187)Re/~(188)Os ratios are characterized by high and variable range of 270.90 to 4 074.99, while their ~(187)Os/~(188)Os ratios are moderately radiogenic, ranging from 0.340 0 to 3.655 7. The Re-Os model ages for the bitumen vary between 28 Ma and 144 Ma, with an average of ~85 Ma. With conbination of the documented geological researches, the paper suggests that the Majiang hydrocarbon deposit should be finally accumulated at ~144 Ma of Indosinian to Early Yanshanian period, and destroyed at ~85 Ma of Late Yanshanian period.