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无机成因

无机成因的相关文献在1986年到2021年内共计103篇,主要集中在石油、天然气工业、地质学、矿业工程 等领域,其中期刊论文98篇、会议论文4篇、专利文献29400篇;相关期刊49种,包括吉林大学学报(地球科学版)、地质通报、高校地质学报等; 相关会议4种,包括2014年中国地球科学联合学术年会、第十一届全国有机地球化学学术会议、第十届全国有机地球化学学术会议等;无机成因的相关文献由239位作者贡献,包括张景廉、戴金星、刘德良等。

无机成因—发文量

期刊论文>

论文:98 占比:0.33%

会议论文>

论文:4 占比:0.01%

专利文献>

论文:29400 占比:99.65%

总计:29502篇

无机成因—发文趋势图

无机成因

-研究学者

  • 张景廉
  • 戴金星
  • 刘德良
  • 崔永强
  • 郭占谦
  • 卫平生
  • 张虎权
  • 杨晓勇
  • 刘嘉麒
  • 刘立
  • 期刊论文
  • 会议论文
  • 专利文献

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    • 罗群; 贾春; 欧光习; 梁光河; 刘银河; 曾普胜; 陈佳宇; 崔倩
    • 摘要: 明确油气的成因及其分布具有重要的理论与现实意义.针对目前石油成因研究中的关键科学问题,以全球构造学、石油地质学的一般原理为指导,对各种石油成因假说进行梳理、融合和集成创新,形成了石油的双机(有机—无机)耦合成因假说框架.其主要观点是,石油(或天然气)是一种多成因的可再生资源,储量巨大.石油的形成与分布是盆地与地幔隆起、深部流体与浅部流体、有机生烃机制与无机生烃机制、深大断裂与封盖条件4对成烃成藏要素相互耦合的结果.双机耦合程度越好,油气越丰富.盆地及其基底以下区域是耦合程度最好的领域,其次是盆地周边区域封盖条件较好的深大断裂发育区;深大断裂与封盖条件的匹配是控制油气聚集的重要因素;长期、多期或近期活跃的深大断裂发育区封盖条件好的大型圈闭,是最可能取得重大勘探突破的区域.
    • 赵厚祥
    • 摘要: 非烃气成因类型的研究与烃类气的生成、运移、聚集成藏有密切联系.瑞宝盆地天然气具有有机成因烃类气与无机成因烃类气、非烃气混源特征;烃类气以甲烷为主;非烃气为N2、H2、CO2、CO及H2S;利用单因子(δ13C1或δ13Cco2)方法判别天然气成因存在一定偏差,δ13Cco2-δ13C1、δ13C1-R0等二元关系图版并考虑沉积背景综合判别效果好;有机成因烃类气主要来源于煤系烃源岩,有机成因非烃气主要来源于煤和干酪根的热解;无机成因烃类气、非烃气主要来源于碳酸盐岩的高温还原作用和火山活动.控盆深大断裂及火山岩的空间分布规律是控制非烃气富集的主要因素.非烃气的赋存对烃源岩的演化、油气运移聚集、储层质量以及成藏组合都有积极的地质指向意义.
    • 王旭; 赵其华; 邓庆; 梁玉飞
    • 摘要: In order to learn the formation mechanism and developing characteristics of unknown gas in a tunnel on Sichuan-Tibet Railway and to find a new method for study of unknown gas,the study methods for engineering geology and geochemistry are analyzed.The unknown gas,the mixed gas,is identified according to sample test,all-weather monitoring data and study of the formation mechanism and developing characteristics of the unknown gas.And then,the possible migration of the unknown gas from other regions is eliminated according to the study of engineering geology,the distributions and geological structures of gas resources and coal-bearing strata and rock fissure developing conditions.Finally,the laboratory test and geochemical analysis are carried out on rock sample,which demonstrate the organic and inorganic formation mechanisms,small storage and the autochthonous generation of the unknown gas.The study can provide reference for followed successful construction of the tunnel.%为解决复杂地质条件地区隧道工程建设中出现的不明气体问题,以川藏铁路某隧道出现不明气体为切入点,结合工程地质学、地球化学等学科交叉的研究方法与思路,对该不明气体的成因机制及演化特征进行研究,探索一种研究不明气体的新思路.基于现场采样测试与全天候监测,总结分析该不明气体成分特征及其演化规律,得出该不明气体为混合成因气体;同时,从不明气体的工程地质条件入手,着眼于区域油气资源和煤系地层的分布及区域地质构造、岩石裂隙发育情况,排除不明气体由其他地区运移而来的可能;在此基础上,进行岩石室内试验,通过对不明气体赋存环境进行地球化学分析,分别论证气体的有机成因及无机成因,得出该不明气体是原地产生的,经历了有机成因和无机成因2个阶段且储量有限,对工程后期影响不大,为隧道后期顺利施工提供了指导.
    • 舒思齐; 张洪涛; 肖序常
    • 摘要: 基于超基性岩蛇纹石化成油理论,根据构造条件和沉积条件,提出了石油勘查概念模型——“BRCF”模型:B代表侵入地壳超基性岩;R代表储油层;C代表盖层;F代表深大断裂.运用该模型分析了波斯湾地区油气田和中国典型油气田油气成藏规律,并预测了中国大陆油气勘查靶区.%According to the tectonic setting and sedimentary condition,the conceptual model of oil and gas exploration,"BRCF" model,is built on the basis of the origin theory of serpentinized ultrabasic rocks.B is the ultrabasic rocks intruding the earth's crust.R is the oil-bearing reservoir.C is the cap rock.F is deep fracture.The model was used to analyze the reservoir-forming regularity of typical oil and gas fields in Persian Gulf and China's continent and to predict the oil and gas targets in China's continent.
    • 王旭1; 赵其华12; 邓庆1; 梁玉飞1
    • 摘要: 为解决复杂地质条件地区隧道工程建设中出现的不明气体问题,以川藏铁路某隧道出现不明气体为切入点,结合工程地质学、地球化学等学科交叉的研究方法与思路,对该不明气体的成因机制及演化特征进行研究,探索一种研究不明气体的新思路。基于现场采样测试与全天候监测,总结分析该不明气体成分特征及其演化规律,得出该不明气体为混合成因气体;同时,从不明气体的工程地质条件入手,着眼于区域油气资源和煤系地层的分布及区域地质构造、岩石裂隙发育情况,排除不明气体由其他地区运移而来的可能;在此基础上,进行岩石室内试验,通过对不明气体赋存环境进行地球化学分析,分别论证气体的有机成因及无机成因,得出该不明气体是原地产生的,经历了有机成因和无机成因2个阶段且储量有限,对工程后期影响不大,为隧道后期顺利施工提供了指导。
    • 陈义林; 秦勇
    • 摘要: Gaseous carbon dioxide (CO2) in natural gas and dissolved inorganic carbon (DIC) in aqueous system are in chemical and isotopic equilibrium.A gas-water exchange experiment with inorganic gaseous CO2 in a closed glass bottle was performed to elucidate the meticulous dynamic change in the chemical composition when gaseous CO2 dissolves in the water.The results indicate that the CO2 gas achieved compositional and carbon isotopic equilibrium through the gas-water interface within 13 h at 101 325 Pa and 30 °C.The initial concentration and δ13Cco2 values of gaseous CO2 were 2.0% and-2.5%,respectively,and the equilibrium values were 1.1% and-14.6%,respectively,with a strong isotopic fractionation (i.e.,12.1%).During the gas-water exchange and dissolution of CO2,the CO2 concentration and δ13Cco2 values could be expressed as an exponential function of time.The δ13CDIC value,which was approximately-8.2%,indicated that a larger proportion of DIC came from organic origin.Gaseous inorganic CO2 was mixed by organic CO2 in water through the gas-water interface,which ultimately presented the characteristic of organic gas.Therefore,carbon isotopic geochemistry of groundwater must be investigated prior to determining the origin and source of gaseous CO2 in natural gas.%天然气中二氧化碳组分和水体中溶解无机碳构成碳酸平衡体系及碳同位素分馏平衡体系.通过开展无机成因二氧化碳气体的气-水交换实验,揭示了二氧化碳气体在溶解过程中组分体积分数和碳同位素的精细变化.研究发现:在101 325 Pa和30°C条件下,二氧化碳气体经13 h与瓶中水体达到组分体积分数和碳同位素的分馏平衡;初始二氧化碳体积分数为2.0%,平衡后为1.1%;初始613C CO2值为-2.5%,平衡后为-14.6%,碳同位素分馏幅度高达12.1%.经气-水界面交换反应,无机成因二氧化碳气体体积分数和碳同位素值随时间变化均可表征为负指数函数.黄河水样δ13CDIC值为-8.2%,表明水体中大部分DIC来源于土壤有机质分解释放的CO2;富重碳同位素二氧化碳气体与水体DIC反应平衡后,二氧化碳气体由无机成因经混染改造为有机成因.
    • 滕吉文; 刘有山; 乔勇虎
    • 摘要: The origin of oil and gas affects not only the configuration of energy structure in our country even the whole world but also the position and orientation of energy in social and economic development.Since the 17th century,the debate on the organic and inorganic origins of oil has lasted about 300~400 years.Although the organic origin has been a dominant theory over the inorganic origin,the latter is flourishing constantly.Based on scholars' understanding and study over the past few hundred years,in theory,both of them have their own material basis and arguments.However,it is too early or inappropriate to deny the thesis and argument of inorganic origin of oil and gas on the basis of some facts.For instance,the trace metal elements accumulate and dissipate in the source-reservoir environments of some specific oil fields throughout the world,the porphyrin molecular cannot be found as biomarkers in some oil fields,the hydrocarbon-oxidation chemical synthesis of oil achieve some development and so forth.Obviously,it is possible for the inorganic oil to migrate and permeate into the reservoirs of oil fields under the condition that the organic oil is a dominant body.Based on the above analysis,study and exploration,we propose a new idea,i.e.the hybrid origin of oil and gas (a organic origin + b inorganic origin).We sincerely hope that this new idea can be studied and explored throughout the development of oil industry in theory,technology,experiments and practice,which will be beneficial to understanding and expanding the reservoir space of oil and gas.%石油与天然气的成因问题关系到我国乃至世界各国能源结构的配置及其能源在社会与经济发展中的地位和导向.自从17世纪展开对石油的有机与无机成因的争论以来,至今已有约300~400年的历史.尽管有机成因论占据了统治地位,但是无机成因论亦不断地在兴起!通过对这二者的理解和研究,从理论上讲他们都具有一定的物质基础和论据.基于对国内、外一些特异油田的生储环境,原油中所富含的微量金属元素的聚集与散失,某些油田中并未找到卟啉分子这样的生物标志物,碳、氢、氧化学合成实验等方面取得了一定的成效,故全盘否定无机生油的论点和论据确尚感为时过早或欠妥!显然,在以有机物成油为主体的前提下,无机物亦可生成部分石油,并通过运移、渗透到各油田的储集层中应是完全可能的.基于这样的分析、研究和探索,现提出石油的双机(a有机+b无机)混合成因的新理念.诚希能在今后的石油工业发展中,从理论、技术、实验和实践中强化对双机混合成因新理念的深化研究与探索,以达深切理解和扩展石油生、储空间环境等是不无裨益的!
    • 陈银节; 汤玉平; 黄欣
    • 摘要: The Changde gas reservoir in the Songliao Basin is the only inorganic gas reservoir in the world which mainly produces alkane gas with a full geochemical complement. Therefore, the study of Changde inorganic gas reservoir has a great significance for the development of China’s natural gas exploration. We designed a geochemical profile crossing wells Fangshen1 and Fangshen2 above the Changde gas reservoir, studied the near⁃surface display of different geochemical indicators, and selected effective geochemical methods and abnormal indicators. The analysis of methane carbon isotopes can help judge the inorganic origin of the reservoir.%松辽盆地昌德气藏是目前世界上发现的唯一有充分地球化学依据,以产烷烃气为主的无机成因气藏。加强对昌德无机气藏的解剖,对于拓展我国天然气的勘探领域,具有重要意义。在昌德气藏上方,布置了一条贯穿芳深1井和芳深2井的地球化学剖面,通过研究不同地球化学指标在气藏上方的显示特征,确定了昌德气藏有效地球化学方法组合及异常识别标志。同时,结合甲烷碳同位素的分析,可以从一定程度上判断下伏气藏的无机成因属性。
    • 尚尧; 施尚明
    • 摘要: 以试气井段为单位对徐家围子断陷深层天然气进行分析,探索各气藏天然气组成及碳同位素的分布规律.研究表明:乙烷碳同位素在平面上存在明显差异,断陷边部乙烷碳同位素较重,具有煤型气特征,断陷中部乙烷碳同位素较轻,达到油型气标准;天然气C5以上的重烃碳同位素异常轻,可能来源于原油裂解;碳同位素反序的天然气不一定是无机成因,复杂的碳同位素序列可能是油型气和煤型气混合造成;无机成因烃气数量甚微,不可能单独成藏.
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