地球化学资料定量识别层序地层单元技术综述Methods to Recognize Sequence Stratigraphic Units Based on the Geochemistry Data
朱红涛;庄文娟;黄众;刘强虎;
摘要(Abstract):
应用地球化学资料识别层序地层单元的方法包括:碳氧同位素法、黏土矿物法、胶结物含量法、微量元素法、稀土元素法、TOC识别法、镜质体反射率法等。上述方法识别层序地层单元具有识别准确和分辨率高等优点,缺点是容易受到样品采样不连续的限制和受成岩作用、岩浆作用、构造作用等其他因素的影响。因此,在多地球化学指标结合识别层序地层单元的基础上,还应结合测井、地震、古生物等资料开展层序地层单元综合识别。
关键词(KeyWords): 层序地层单元;地球化学资料;微量元素法;黏土矿物法;综合方法
基金项目(Foundation): 国家科技重大专项课题(2011ZX05030-002-002);; 国家自然科学基金项目(40702024);; 霍英东教育基金项目(132020);; 中央高校基本科研业务费专项资金资助项目(CUGL100412);; 教育部留学回国人员科研启动基金项目(2009022014)
作者(Author): 朱红涛;庄文娟;黄众;刘强虎;
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DOI:
参考文献(References):
- [1]郑荣才,彭军,吴朝荣.陆相盆地基准面旋回的级次划分和研究意义[J].沉积学报,2001,19(2):249-255.
- [2]赵俊青,纪友亮,张世奇,等.陆相高分辨率层序界面识别的地球化学方法[J].沉积学报,2004,22(1):79-86.
- [3]Spezzaferri S,McKenzie J A,Isern A.Linking the oxygen i-sotope record of late Neogene eustasy to sequence stratigraphicpatterns along the Bahamas margin:Results from a paleocean-ographic study of ODP Leg 166,Site 1006sediments[J].Ma-rine Geology,2002,185:95-120.
- [4]李家华,旷红伟,彭楠,等.冀北宽城中元古界杨庄组地球化学特征[J].岩石矿物学杂志,2010,29(3):289-297.
- [5]Elrick M,Garza R M,Duncan R.C-isotope stratigraphy andpaleoenvironmental changes across OAE2(mid-Cretaceous)from shallow-water platform carbonates of southern Mexico[J].Earth and Planetary Science Letters,2009,277:295-306.
- [6]Jarvis I,Murphy A M,Gale A S.Geochemistry of pelagic andhemipelagic carbonates:Criteria for identifying systems tractsand sea-level change[J].Journal of the Geological Society,2001,158(4):685-696.
- [7]董红梅,宋友桂.黏土矿物在古环境重建中的应用[J].海洋地质与第四纪地质,2009,29(6):119-130.
- [8]Albani A E,Meunier A,Macchiarelli R.Local environmentalchanges recorded by clay minerals in a karst deposit duringMIS 3(La Chauverie,SW France)[J].Quaternary Interna-tional,2011,241:26-34.
- [9]白斌,邹才能,朱如凯,等.利用露头、自然伽马、岩石地球化学和测井地震一体化综合厘定层序界面:以四川盆地上三叠统须家河组为例[J].天然气地球科学,2010,21(1):78-86.
- [10]Ketzer J M,Morad S,Evans R,et al.Distribution of diage-netic alterations in fluvial,deltaic,and shallow marine sand-stones within a sequence stratigraphic framework:Evidencefrom the Mullaghmore Formation(Carboniferous),NW Ireland[J].Journal of Sedimentary Research,2002,72(6):760-774.
- [11]韩登林,张昌明,尹太举.层序界面成岩反应规律及其对储层储集物性的影响[J].石油与天然气地质,2010,31(4):450-454.
- [12]刘刚,周东升.微量元素分析在判别沉积环境中的应用[J].石油实验地质,2007,29(3):307-314.
- [13]Nagy J,Hess S,Dypvik H,et al.Marine shelf to paralic bio-facies of Upper Triassic to Lower Jurassic deposits in Spitsber-gen[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2011,300:138-151.
- [14]Legler B,Schneider J W,Gebhardt U,et al.Lake deposits ofmoderate salinity as sensitive indicators of lake level uctua-tions:Example from the Upper Rotliegend saline lake(Middle-Late Permian,Northeast Germany)[J].Sedimentary Geology,2011,234:56-69.
- [15]罗顺社,汪凯明.元素地球化学特征在识别碳酸盐岩层序界面中的应用:以冀北坳陷中元古界高于庄组为例[J].中国地质,2010,37(2):430-438.
- [16]龙天才.关于应用硼判别沉积环境的有效性问题[C]∥佚名.第四纪冰川与第四纪地质论文集(5).北京:地质出版社,1988:233-235.
- [17]张金亮,张鑫.塔里木盆地志留系古海洋沉积环境的元素地球化学特征[J].中国海洋大学学报,2006,36(2):200-208
- [18]Walker C T,Price N B.Departure curves for computing pal-eosalinity from boron in illites and shales[J].AAPG,1963,47(5):833-841.
- [19]Adams T D,Haynes J R,Walker C T.Boron in Holocene ilitesof the dovey estuary wales and its relationship to paleosalinityin eyeleothems[J].Sedimentology,1965,4:189-195.
- [20]Nelson B.Sedimentary phosphate method for estimating pal-eosalinities[J].Science,1967,158:917-920.
- [21]熊小辉,肖加飞.沉积环境的地球化学示踪[J].地球与环境,2011,39(3):405-414.
- [22]朱建明,朱祥坤,黄方.钼的稳定同位素体系及其地质应用[J].岩石矿物学杂志,2008,27(4):353-360.
- [23]周炼,苏洁,黄俊华,等.判识缺氧事件的地球化学新标志:钼同位素[J].中国科学:地球科学,2011,41(3):309-319.
- [24]吴仕强,朱井泉,胡文瑄.塔里木盆地寒武系—奥陶系白云岩稀土元素特征及其成因意义[J].现代地质,2009,23(4):638-647.
- [25]蓝先宏,申顺喜.南海中部沉积岩心的稀土元素地球化学特征[J].海洋通报,2002,21(5):46-55.
- [26]杨国臣,于炳松,陈建强,等.川西前陆盆地上侏罗统—白垩系泥质岩稀土元素地球化学[J].现代地质,2010,24(1):140-150.
- [27]孙蓓蕾,曾凡桂,李美芬.西山煤田马兰矿区8号煤及其夹矸的微量与稀土元素地球化学特征[J].煤炭学报,2010,35(1):110-116.
- [28]赵志根,唐修义,李宝芳.淮南矿区煤的稀土元素地球化学[J].沉积学报,2000,18(3):453-459.
- [29]龚玲兰,奚小双,孔华,等.湘江悬浮物的稀土元素地球化学研究[J].沉积学报,2009,27(3):529-536.
- [30]杨守业,李从先.REE示踪沉积物物源研究进展[J].地球科学进展,1999,14(2):164-167.
- [31]黄舜华,章钟嵋,何松裕,等.稀土元素在海水中的运移形式与沉淀条件的某些实验研究[J].地球化学,1981,4:398-406.
- [32]汪涌,操应长,郑文涛,等.陆相深水沉积层序和体系域边界识别方法初探:以东营凹陷牛38井为例[J].现代地质,2004,18(2):181-184.
- [33]张立强,罗晓容,何登发,等.准噶尔盆地南缘下白垩统层序界面的识别[J].沉积学报,2004,22(4):637-643.
- [34]Khoshnoodkia M,Mohseni H,Rahmani O,et al.TOC deter-mination of Gadvan Formation in South Pars Gas Field,usingartifical intelligent systems and geochemical data[J].Journal ofPetroleum Science and Engineering,2011,78:119-130.
- [35]刘招君,孙平昌,贾建亮,等.陆相深水环境层序识别标志及成因解释:以松辽盆地青山口组为例[J].地学前缘,2011,18(4):171-180.
- [36]Creaney S,Passey Q R.Recurring patterns of total organic-carbon and source rock quality within a sequence stratigraphicframework[J].AAPG Bulletin,1993,77(3):386-401.
- [37]王敏芳,黄传炎,徐志诚,等.浅述地层剥蚀量恢复的基本原理与方法[J].海洋石油,2006,26(1):28-33.
- [38]王曦,万晓樵,李国彪.西藏岗巴晚白垩世—古近纪早期锶同位素地层[J].中国地质,2008,35(4):598-607.
- [39]Wickman F E.Isotope ratios:A clue to the age of certain ma-rine sediments[J].Geology,1948,56:61-66.
- [40]Hannigan R,Brook M E,Basu A R.A detailed 87Sr/86Sr iso-topic curve for the mid-Cincinnatian(Upper Katian-LowerHirnantian,Upper Ordovician),NE North American Shelf(Ontario,Canada)transition to the Hirnantian glaciation[J].Chemical Geology,2010,277:336-344.
- [41]Munnecke A,Calner M,David A T.Ordovician and Siluriansea-water chemistry,sea level,and climate:A synopsis[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,296:389-413.
- [42]张萌,黄思静,张玥,等.锶同位素地层学在海相地层定年中的潜在价值[J].成都理工大学学报:自然科学版,2003,30(3):242-247.
- [43]李荣西,魏家庸,杨卫东,等.用87Sr/86Sr研究海平面变化与全球对比问题[J].地球科学进展,2000,15(6):729-733.
- [44]杨立成,朱莎.锶同位素的几种应用[J].中国西部科技,2010,9(28):27-28.
- [45]吴因业,朱如凯,罗平.沉积学与层序地层学研究新进展:第18届国际沉积学大会综述[J].沉积学报,2011,29(1):200-205.
- [46]肖宗林,沈忠民,许建喜,等.碳酸盐岩层序地层学回顾与展望[J].重庆科技学院学报:自然科学版,2011,13(2):69-71.
- [47]何学贤,李世珍,唐索寒.Mg同位素应用研究进展[J].岩石矿物学杂志,2008,27(5):472-476.
- [48]赫云兰,刘波,秦善.白云石化机理与白云岩成因问题研究[J].北京大学学报:自然科学版,2010,2:53-63.
- [49]李国蓉,曾允孚,周心怀,等.十万大山地区下-中泥盆统白云岩成岩层序地层学研究[J].成都理工大学学报:自然科学版,2004,31(6):668-671.
- [50]郑荣才,刘文均,李祥辉.白云岩成因在层序地层研究中的应用:以龙门山泥盆系为例[J].矿物岩石,1996,16(1):28-37.
- [51]陈辉,田景春,张翔,等.川东北地区下三叠统飞仙关组鲕滩白云岩成因[J].天然气工业,2008,28(1):42-47.