Combined evidence from the outcrop and the fluid inclusion assemblage (FIA) analysis indicates that there exist two episodes of fluid flow controlled by the tectonic activity. The first episode was recorded mainly in ...Combined evidence from the outcrop and the fluid inclusion assemblage (FIA) analysis indicates that there exist two episodes of fluid flow controlled by the tectonic activity. The first episode was recorded mainly in the reservoir rock of the Honghuayuan Formation,representing the fluid flow of hydrocarbon charging. The second episode occurred mainly along the fault systems,representing the fluid move-ment when the ancient oil reservoir was destroyed. The host mineral morphology,homogeneous tem-perature,and salinity of the FIAs record an episodic fluid movement. Characters of high homogenous temperature,low salinity and a quick temperature variation of the first episode fluid flow may indicate an early-stage fluid eruption,and correspondingly,fine-grained calcite was formed. Temperature of the erupted fluid tended to decrease during its mixing with the upper formation fluid and finally had the same temperature as the upper formation. From then on,the temperature was rather steady and fa-vored the growth of the coarse calcite. Due to this character of the temperature variation of the episodic fluid flow,we can use the homogenous temperature of the FIA of the coarse calcite to date the forma-tion and the destruction time of the Majiang ancient oil reservoir. Episodic fluid flow was known for its inhomogeneous trapping,which resulted in the failure of dating according to the burial history. But taking a close look at its temperature variation,we think that the latest stage of fluid flow,characterized by steady state temperature and grow of the coarser crystals,can be used for dating. It will be of great value if this method is proved to be effective. The formation and the destruction time of the Majiang ancient oil reservoir were dated to be in the Indosinian Period and the late Yanshan-early Hymalayan Period respectively. This conclusion is in great discrepancy with the common accepted idea that the Majiang ancient oil reservoir was formed and destroyed during the Caledonian tectonic movement. Even so,this paper further discussed its reliability from the view of the source rock evolution and also the local tectonic evolution.展开更多
IN nature, there are many coexisting examples of petroleum with metallic ore deposit. There are metallicore deposits in the border and interior of many petroliferous basins, such as the bedded Pb-Zn ore depositin carb...IN nature, there are many coexisting examples of petroleum with metallic ore deposit. There are metallicore deposits in the border and interior of many petroliferous basins, such as the bedded Pb-Zn ore depositin carbonate rock, gold sulfide ore deposit in black shale, cinnabar deposit, copper sandstone, kupferschiefer ore deposit, etc. (Tang Kuilian, 1995). The liquid hydrocarbon all was found in the Pb-Zn oredeposit, Mercury deposit, Carlin gold deposit (Shi Jixi et al., 1995) as well as the beds adjacentto them. There are a large number of bitumen and organic inclusions with hydrocarbon in the low-temperature Hg-Sb-Au ore concentrated district in southwestern margin to Yangtze platform. Fu Jiamao (1988)thought that they are remains after the ancient oil reservior destructed. In pace with constantly finding thecoexisting phenomena of metallic ore deposit and petroleum as well as further studying the relationship between both of them, it is progressively known that there are close links between oil/gas field and展开更多
The GOI（grains containing oil inclusions） index is used to distinguish oil zones,oil-water zones and water zones in sandstone oil reservoirs.However,this method cannot be directly applied to carbonate rocks that may...The GOI（grains containing oil inclusions） index is used to distinguish oil zones,oil-water zones and water zones in sandstone oil reservoirs.However,this method cannot be directly applied to carbonate rocks that may not have clear granular textures.In this paper we propose the Effective Grid Containing Oil Inclusions（EGOI） method for carbonate reservoirs.A microscopic view under10× ocular and 10 x objective is divided into 10×10 grids,each with an area of 0.0625 mm×0.0625 mm.An effective grid is defined as one that is cut（touched） by a stylolite,a healed fracture,a vein,or a pore-filling material.EGOI is defined as the number of effective grids containing oil inclusions divided by the total number of effective grids multiplied by 100%.Based on data from the Tarim Basin,the EGOI values indicative of the paleo-oil zones,oil-water zones,and water zones are 〉5%,1%-5%,and 〈1%,respectively.However,the oil zones in young reservoirs（charged in the Himalayan） generally have lower EGOI values,typically 3%-5%.展开更多
华南板块新元古代的兴凯地裂运动始于晋宁运动后(800 Ma B.P.),强烈活动于新元古代中期的苏雄—开建桥组火山岩喷发期(700 Ma B.P.),结束于中奥陶世的郁南运动(458 Ma B.P.)。演化历程大体相当于Rodinia(罗迪尼亚)超大陆解体时,应为Rodi...华南板块新元古代的兴凯地裂运动始于晋宁运动后(800 Ma B.P.),强烈活动于新元古代中期的苏雄—开建桥组火山岩喷发期(700 Ma B.P.),结束于中奥陶世的郁南运动(458 Ma B.P.)。演化历程大体相当于Rodinia(罗迪尼亚)超大陆解体时,应为Rodinia超大陆裂解期的组成部分。兴凯地裂运动在新元古代形成扬子板块的基底,对中上扬子区后期构造变形有重要的影响,为后兴凯期(加里东运动)形成大型古隆起和大形拗陷提供了基础;产生的基底断裂对四川盆地后期构造活动有控制作用;形成的稳定大陆边缘为下组合烃源岩发育提供了条件等。展开更多
基金Supported by National Basic Research Program of China (Grant No.2006CB202308,2005CB422107)National Natural Science Foundation of China (Grant No.40472078)
文摘Combined evidence from the outcrop and the fluid inclusion assemblage (FIA) analysis indicates that there exist two episodes of fluid flow controlled by the tectonic activity. The first episode was recorded mainly in the reservoir rock of the Honghuayuan Formation,representing the fluid flow of hydrocarbon charging. The second episode occurred mainly along the fault systems,representing the fluid move-ment when the ancient oil reservoir was destroyed. The host mineral morphology,homogeneous tem-perature,and salinity of the FIAs record an episodic fluid movement. Characters of high homogenous temperature,low salinity and a quick temperature variation of the first episode fluid flow may indicate an early-stage fluid eruption,and correspondingly,fine-grained calcite was formed. Temperature of the erupted fluid tended to decrease during its mixing with the upper formation fluid and finally had the same temperature as the upper formation. From then on,the temperature was rather steady and fa-vored the growth of the coarse calcite. Due to this character of the temperature variation of the episodic fluid flow,we can use the homogenous temperature of the FIA of the coarse calcite to date the forma-tion and the destruction time of the Majiang ancient oil reservoir. Episodic fluid flow was known for its inhomogeneous trapping,which resulted in the failure of dating according to the burial history. But taking a close look at its temperature variation,we think that the latest stage of fluid flow,characterized by steady state temperature and grow of the coarser crystals,can be used for dating. It will be of great value if this method is proved to be effective. The formation and the destruction time of the Majiang ancient oil reservoir were dated to be in the Indosinian Period and the late Yanshan-early Hymalayan Period respectively. This conclusion is in great discrepancy with the common accepted idea that the Majiang ancient oil reservoir was formed and destroyed during the Caledonian tectonic movement. Even so,this paper further discussed its reliability from the view of the source rock evolution and also the local tectonic evolution.
文摘IN nature, there are many coexisting examples of petroleum with metallic ore deposit. There are metallicore deposits in the border and interior of many petroliferous basins, such as the bedded Pb-Zn ore depositin carbonate rock, gold sulfide ore deposit in black shale, cinnabar deposit, copper sandstone, kupferschiefer ore deposit, etc. (Tang Kuilian, 1995). The liquid hydrocarbon all was found in the Pb-Zn oredeposit, Mercury deposit, Carlin gold deposit (Shi Jixi et al., 1995) as well as the beds adjacentto them. There are a large number of bitumen and organic inclusions with hydrocarbon in the low-temperature Hg-Sb-Au ore concentrated district in southwestern margin to Yangtze platform. Fu Jiamao (1988)thought that they are remains after the ancient oil reservior destructed. In pace with constantly finding thecoexisting phenomena of metallic ore deposit and petroleum as well as further studying the relationship between both of them, it is progressively known that there are close links between oil/gas field and
基金supported by the project of Research on Fluid Inclusions and Geological Ages of Hydrocarbon Accumulations of Key Reservoirs in the Tarim Basin (No.041014080008)
文摘The GOI（grains containing oil inclusions） index is used to distinguish oil zones,oil-water zones and water zones in sandstone oil reservoirs.However,this method cannot be directly applied to carbonate rocks that may not have clear granular textures.In this paper we propose the Effective Grid Containing Oil Inclusions（EGOI） method for carbonate reservoirs.A microscopic view under10× ocular and 10 x objective is divided into 10×10 grids,each with an area of 0.0625 mm×0.0625 mm.An effective grid is defined as one that is cut（touched） by a stylolite,a healed fracture,a vein,or a pore-filling material.EGOI is defined as the number of effective grids containing oil inclusions divided by the total number of effective grids multiplied by 100%.Based on data from the Tarim Basin,the EGOI values indicative of the paleo-oil zones,oil-water zones,and water zones are 〉5%,1%-5%,and 〈1%,respectively.However,the oil zones in young reservoirs（charged in the Himalayan） generally have lower EGOI values,typically 3%-5%.
文摘华南板块新元古代的兴凯地裂运动始于晋宁运动后(800 Ma B.P.),强烈活动于新元古代中期的苏雄—开建桥组火山岩喷发期(700 Ma B.P.),结束于中奥陶世的郁南运动(458 Ma B.P.)。演化历程大体相当于Rodinia(罗迪尼亚)超大陆解体时,应为Rodinia超大陆裂解期的组成部分。兴凯地裂运动在新元古代形成扬子板块的基底,对中上扬子区后期构造变形有重要的影响,为后兴凯期(加里东运动)形成大型古隆起和大形拗陷提供了基础;产生的基底断裂对四川盆地后期构造活动有控制作用;形成的稳定大陆边缘为下组合烃源岩发育提供了条件等。
