王铁冠
分子有机地球化学、石油地质学、油藏地球化学、环境科学。
个性化签名
- 姓名:王铁冠
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学术头衔:
博士生导师
- 职称:-
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学科领域:
勘查地质学
- 研究兴趣:分子有机地球化学、石油地质学、油藏地球化学、环境科学。
王铁冠, 男, 原籍广东澄海,1937年12月生于上海市。1965年毕业于北京石油学院石油地质专业;1983~1986年在美国特拉华大学地质系和俄勒冈州立大学任研究学者、客座副研究员。现任中国石油大学(北京)教授、博士生导师,兼任教育部石油天然气成藏机理、煤炭资源两个重点实验室的学术委员、中石油股份公司油气地球化学重点实验室学术委员会副主任、《地质学报(英文版)》、《地质论评》、《地球化学》、《石油实验地质》、《海相油气地质》等刊物编委。专业领域分子有机地球化学、石油地质学、油藏地球化学、环境科学。他在科研领域中取得的主要成果有:①发现、鉴定和命名了三个新生物标志物系列(13α正烷基-三环萜烷、甲基三环萜烷和甲基四环萜烷);②建立了低熟油气成因的系统理论,及时推广低熟油理论,取得显著效益;③建立有机地球化学与煤岩学结合的煤系烃源岩研究方法,系统提出烃源岩的I-III型显微组分的非均质性组成,富氢组分“分期生油”的理论;④首次论证含硫非烃二苯并噻吩类,作为新分子标志物示踪石油运移的机理,用以反演石油运移优势通道,展现油藏充注途径;⑤运用流体包裹体测温,结合数值模拟,确定油藏成藏期次与时间;⑥在不同岩性的油藏中,重建油田的成藏历史,预测烃源灶方位,确定有利勘探方向,产生显著经济效益。多年来,他发表论文179篇(含英文43篇),合撰专著13部,译著6部,完成科研报告41份。论著被SCI收录33篇,引用321次。曾获得李四光地质科学奖(地质研究者奖)、中国科学技术发展基金会孙越崎能源大奖、中国石油天然气总公司铁人科技成就奖(银奖)、国家自然科学奖(二等奖)和科技进步奖(三等奖)以及11项部级科技进步奖。
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697
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成果数
10
【期刊论文】Biodegraded Oil and Its High Molecular Weight (C35+) n-alkanes I nthe Q
王铁冠, WANG Tieguan, ZHU Dan, LU Hong, , ZHANG Zhihuan and YANG Chiyin
,-0001,():
-1年11月30日
With a production of 208.2 m3/d, heavy oil was produced by drill stem test (DST) from three shalow reservoirs in Sand Group Nos.1 and UI of the Neogene Guantao Formation 9Ng1 and NgU) and the Eogene Dongying Fornation (Ed) in an explaratory well Ban-14-1 within the Qianmiqiao region, Bohai Bay Basin, northern China, Based on the GC and Gc-MS data of th ND1 and Non1 heavy oil samples, all n-alkanes and mos tisprenoid hydrocabons ared lost andthe GC baseline appears as an eviden "HUMP" implying a large quantity of unresolved complex mixture (UCM), which typically revecaled a result of heavy biodegradation, Howerer, there still is a complete serics of C14-C75 n-alkanes i nthe hightemperature, temperature gas chromatogrands (HTGC) of the heavy oil, arnog which the abundance of C30-n alkanes ate drastically redused The C35-C55 high molecular weight HMW N-alkanes are at high abundance and show a normal distribution pattern withmajor Peak at Cu and obvious odd-carbon-number preddominance with CPI37-55 and OEP 45-49 Values of 1.17 and 1.16-1.20, respectively, According to GC-MS analysis, the heavy oil is characteizxed by dual source inputs of aquatic microbes and terrestial higher plants varous steranes and tricyclcterpanes indicate andalgal origin, and hopane-type triterpanes, C24 tetracyclic terpane anddrmane seriesshow the bacterial contribution, With the odd-carbon-numbwr prefernce, HMY N-alkanes provide xignificand infornnation not only on higher plant source input and immaturity, but also on the strong resisbility foto blodgeradation
high-temperanure gas chromatography (, HTGC), high molecular weighe (, HMW), n-alkane,, biodegradation
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王铁冠, T.-G. Wang a, *, S.-M. Li a, S.-C. Zhang a, b
Journal of Petroleum Science and Engineering 41(2004)123-134,-0001,():
-1年11月30日
The distribution of pymolic nitrogen compounds (carbzoles and benzocarfaziies) in curde oits of the Lunnan region, produced fromOrdovician, Carboaiferous, Triassic and Jurasslereseroirs, are similar in the overall composition, but different in the total andthe relative abundances ofindividual pyrolic compounds, Since it was previously demonstrated that rnost of the Lunnan oils are sourced from the Middle-Upper Ordovician shaly carbonaterocks, and with similar maturity, these analytical results for pyrrolie aitrogen compounds indicate a renardable geochromatographic fractionation efect during oil migration, especially for lateral secondary migraton, Based onour results, we have shown that the migration andentrapment pathway of the Ordovician andCarboniferous oils is diferent from those for Triassic andJrassie oils in theLnnan region, That is the Ordovician andCarboniferous oils migratedInterally from west to east, and their main filling points wee on both southwest sides of th Lunnan andDangtarm Falt-borset Belts, On the other hand, Triassie and Jrassic oits migratedverticall vin falt conduits from the Ordoviciansource kitechen andthen migratedlaterally from north to south.
Pyrolic narogen compounds, Oil migration, Gechromatographic fractionation effect, Tarim Basin
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王铁冠, WANG Tieguan **, WANG Chunjiang , ZHANG Weibiao , SHI Quan , ZHU Lei , and CHEN Junyuan
,-0001,():
-1年11月30日
Totally 19 sanples of typecal Upper Ptoftroacoe-Lower Cansbrians sedmeristry rocks were colbetal and mtalyed for an organic geocbeenical invesugation. Almost all these rocks have high TOCs. Supper-maturaties and similec biomarser diesribution. As an es-coption, howryes, the Sintian Tillte slaves mosch lower TOCs and little phytans and prlatans in comparison with those in other strata, which amplies a very faint photosynthctic process, and a restricted euphotlc zone and quate limited msnlight within the sesimenoary aawater ndowan during the Sinian glaction ags is the wasta Yangze region proving an evidence lor pehoo-oceane envireontent of the Neoproveroise Snowball Earth age
Late Neoproterozole, Early Canbrian, molocular organtic geochemistry, eophotic zone, Snowball Earth, Yangtze re-gion
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王铁冠, T.-G.Wang and B.R.T. Simoneit*
,-0001,():
-1年11月30日
The biomatrker assemblage in the aliphatic fraction of the Tertiary brown coal from Zhoujing mine has been documented in detal. This aliphatic fcaction consists of resin-derived diterpejnord and sesquiterpenold hydrocarbons. Longchain alkanes from vascular plant epicutlicutar wates. and to a lesser extent terrigenous tnterpenes. The huminite reflectance (Ro) and bomarker patameters indicate the hydrocarbons in this brown coal are immature. Thos, resins and waves of higher plants are particularly important for the generation of immature bydrocarbons from brown coal or lignite.
hopanes, terpanes, hydrocarbon
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王铁冠, WANG Tieguan, WANG Feiyu, LU Hong, YANG Chiyin, LIAO Qianjin and Zhou Jiansbeng
,-0001,():
-1年11月30日
A oil flow obtained from the Middle Ordovician Feagfeng Formation carbonate reservoir in the well KG-3, Kongxi burial-hill zone in 1993 marked a breakthrough in petroleum exploration of the high-mature Lower Plaeozoic strata, North China. Both the Lower member of the Fengfeng Formation and the Second Member of the Upper Majiangou Formation in the Middle Ordovician are supposed to be the main source beds. Oil generation peaks range from 1.0% to 1.6% in R. showing a "lag effect" of oil generation in high-mature carbonate soutrce rocks under multicyclic tectonic movement cooditions. The Kongxi burial-bill zone adjoins a potential Ordovician source kitechen, The KG-3 oNTOVICIAN buriat-hill resetvoir has undergone two oil filling events, le. an early event in the Late Carboniferous-Permian and a more significant late event in the carly Eogene.
burial-hill reservolt, source tocks, ", lag effect", , oil-source cotrelation, oil eatrapment epoch
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【期刊论文】Immature Oils in China and Their Genetic Mechanisms
王铁冠, WANG Tieguan
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-1年11月30日
Immature crade oils are a kind of unconyentional petroleum resources. They are generated through early tow-temperature biochemical chemical reactions of some specifie organic rafter. Their geological reserves ex-plored are as high as several hundred milltion tons in China. Based on a dctailed organic geochemical study, five ge-netic mechanisms of immature oils have been proposed in this paper for early bydrocarbon generation from suberinite,, resinlte, tacteria-rewocked terrestrial organic matter, biolipids and sulhur-tich macromolecules respectively.
immature oil, genehc mechanism, bydrocarton generation model
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王铁冠, WANG Tieguan (t.g. wang. 王铁冠), HOU Dujie (侯读杰), ZHONG Ningning (钟宁宁), BAO Jianping (包建平), HUANG Guanghui (黄光辉), ZHANG Linye (张林晔), CHEN Zhilin (陈致林), and LI Peizhen (李佩珍)
,-0001,():
-1年11月30日
Taking both enstern Linqing Deresaion and North Jingsu Besin on Exatoples. Based an grochen, based on geocheraical features of immantre cals as well as source inpots of hydrocartons and macerals, at is revealed that a mixed source input of alga bio-Epids and higher plant warns is a basie chuarieratic of sourte analanial for immoture oil in non-marine brackish-seline lactistrine besits
bio-Hpids, higher plant waxes, hydrocarbon source input, thermo-simulation expcriment, hydrocarbon generatlon model.,
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【期刊论文】Extended 8β (H)-Drimane and 8,14-Secohopane Series in a Chinese Boghead Coal
王铁冠, T.-G. Wang B.R.T Simoneit* R.P.Philp and C.P.Yu
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-1年11月30日
Extended C.,-C23 8β (H)-drimane and C27-C22 8, 14-secohopane series have been detected and identified in a Jurassic boghead coal from Lulong, Hebei, North China, by GC-MS and GC-MS/MS analysis and absed on comparison with reference data and interpretation of mass spectra. The boghead coal is composed of alginite macerats and contains biomarkers of algal and microbial origins such as tricyclie terpanes, hopanes. regeane, and steranes It is proposeed that hte extended 8β (H)-srimane series most likely originates from multiple ptecutrsors i.e. trieyclic terpanes. 8, 14-secohopanes, and hopanes. by opening and/or cleavage of ring C. and an overlll schem is pressented for their posible gendsis
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【期刊论文】燕山东段上元古界含沥青砂岩中一个新三环萜烷系列生物标志物*
王铁冠
,-0001,():
-1年11月30日
本文论述了从燕山东段元古界下马岭组底砂岩古油藏储层沥青中, 检测出来的一个新发现的C12-23三环萜烷系列(质谱基峰m/z123),经人工合成标样注和GC-MS分析,确认其结构为13a(正烷基)-三环匝萜烷,文中结合该储层沥青的生物标志物组合,探讨了其有机母质生源构成、两种降解作用影响,以及新三环萜烷系列的成因。
元古界古藏, 13a(正烷荟)-三环萜烷系列, 脱氢二萜类, 生源构成
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【期刊论文】Organic geochemical evidence for a regional stratigraphic thermal event in East China
王铁冠, T.-G. Wang a, *, Bao Jianping b, B.R.T. Simoneit c
Jounal of Asean Earth Sciences 20(2002)913-930,-0001,():
-1年11月30日
A systemaitic investigation of the pertroleum exploratory welll N-13 within the Huangqiao region, Lower Yangtze Basin, East China, has been carried using multipte analytical techniques of organic geochemistry. The past occurrence of a thermal event has been recognized based on changes in optical vitrinited reflectance (R), pyrolysis peak temperature (Tmo) and chemical hydrogen indes (III), potential degradution rate (D), the atomic H/C ratio and dimethylphenanthrene ratios (DPR.DPR) in the sedimentary mcks. The geological signifience of the thermal event is discvssed in this paper.
Pyrotysis peak temperafure, Chesecal hydrogen index, Ikonogencets geovhernal gredkis
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