芨芨湖西煤矿西山窑组层序地层划分及沉积环境演化特征浅析     

王昭晖  李新光  许平  高永峰  雷国明 《新疆地质》2011,29(1):86-89

通过对煤层分布、特征研究,运用Vail经典层序地层学原理和技术方法,对西山窑组进行层序地层学划分,确定区内西山窑组划分为2个三级层序、6个体系域及10个准层序.提出低位体系域发育断续分布的薄煤层,湖浸和高位体系域发育连续分布的厚煤层和特厚煤层.  相似文献   

扬子地块西北缘二叠系-中三叠统层序地层与沉积相展布   总被引：1，自引：0，他引：1  

魏国齐  杨威  万怡平  金惠 《岩石学报》2011,27(3):741-748

扬子地块西北缘二叠系-中三叠统以大套碳酸盐岩地层为主。本文应用碳酸盐岩层序地层学理论和方法,通过地震、露头、岩心和测井资料分析,在二叠系-中三叠统识别出升隆侵蚀不整合面、海侵上超层序不整合面、水下沉积间断层序不整合面、局部暴露层序不整合面等4种沉积层序界面,并将二叠系-中三叠统划分为11个三级层序23个体系域。通过层序地层对比,建立了研究区层序地层格架,在格架内分析了不同体系域的沉积相特征,认为台缘礁滩相和台内滩相为有利储集相带,且前者主要发育于层序Ⅰ的高位体系域(栖霞组),以及层序Ⅴ和层序Ⅵ的海浸体系域(长兴组和飞仙关组)。  相似文献   

一株H_5亚型禽流感病毒血凝素基因的克隆与序列分析     

高志杰  梁秋婵  刘铀  陈绍红 《广东海洋大学学报》2007,27(3):107-111

根据GenBank中发表的H5亚型禽流感病毒HA基因序列设计2对引物,用RT-PCR方法从禽流感病毒广东分离病毒株(A/Chicken/Guangdong/1997)中扩增HA基因cDNA片段,并将其克隆至pMD-18T载体进行核苷酸序列测定。结果表明:用2对引物所扩增的片段大小分别约为1300 bp和800 bp,经序列拼接获得的HA基因cDNA长度约为1601 bp,编码533个氨基酸,与国内己发表的11个代表株的核苷酸和氨基酸序列同源性为分别为96.9%~99.9%和86.5%~93.0%;HA基因编码的氨基酸序列的系统进化树也表明A/Chicken/Guang-dong/1997、A/Goose/Huadong/01/2000、A/Ck/Hk/37.4/2002、A/Chicken/Zhoukou/2/02、A/Duck/Guangxi/53/2002、A/Duck/Fujian/01/2002等毒株处于同一进化枝,亲缘关系较近;而与A/Silly/Chicken/Hongkong/SF189/01株处于不同进化枝,亲缘关系较远。  相似文献   

新疆于田地区背景地震与触发地震活动分析     

张盛峰  张永仙  庄建仓 《地震地磁观测与研究》2021,42(2):123-124

正新疆于田地区历史上发生过多次6.0级以上地震,北京时间2020年6月26日在此地区再次发生MS 6.4地震。震后,中国地震局地震预测研究所紧急开展地震应急会商,并组织多家单位针对此次地震开展了虚拟科考工作。其中,所发生的地震是否属于其他强震的余震,与历史上已发生的多个强震存在怎样的关系,或者还是属于独立的背景地震活动,  相似文献   

库拜煤田露头层序地层学分析     

陈新蔚  李绍虎  方庆新  阿力木江·吐斯依  李宝庆  马风华 《新疆地质》2013,(1):77-82

通过对库拜煤田阿艾村和音西煤矿侏罗系煤系地层观察、实测露头岩性、沉积构造、特征标志、关键界面等方法,划分沉积亚相、沉积相,按垂向组合特征划分体系域单元.在下侏罗统塔里奇克组至中侏罗统克孜勒努尔组划分出5个沉积层序,从中寻找煤层发育有利层位,总结聚煤规律性.对最大水泛面作为沉积层序关键参照界面依据进行讨论.  相似文献   

伊宁凹陷金鑫煤矿侏罗系露头剖面层序地层分析     

庄新国  李绍虎  马小平  王立民  李宝庆  付黎明  潘力川 《新疆地质》2013,(1):83-88

以伊宁凹陷北缘霍城县金鑫煤矿侏罗系露头地层剖面为研究对象,采用层序地层学和沉积相分析方法,对其层序界面特征、层序的构成特征和沉积相类型进行研究.结果表明,侏罗系露头剖面发育冲积扇、辫状河、曲流河、三角洲和滨浅湖等沉积相类型;层序界面以侵蚀不整合面和河道强烈侵蚀下切面为识别标志.依据确定的层序界面,在八道湾组中划分3个层序、三工河组和西山窑组中分别划分2个层序.低位体系域主要发育冲积扇和辫状河沉积体系,湖扩体系域主要发育滨浅湖沉积,高位体系域主要发育三角洲和曲流河沉积体系.泥炭沼泽主要发育于湖扩体系域和高位体系域.  相似文献   

Environmental and sequence stratigraphic implications of anhydrite textures: A case from the Lower Triassic of the Central Persian Gulf     

《Journal of Asian Earth Sciences》2013

The Lower Triassic Kangan Formation in the Persian Gulf (South Pars Gas Field) and its adjacent areas are composed of carbonate–evaporite sequences. These sediments were deposited in a shallow marine homoclinal ramp. Study of the anhydrite-bearing intervals shows various structures and textures. The anhydrite structures are mainly bedded, massive, chicken-wire and nodular type and the main textures are felted, sparse crystal, needle shape, lath shape, equant and fibrous. Pervasive and poikilotopic cement together with replacement and porphyroblastic gypsum are accounted as the most common diagenetic features in anhydrite. Evaluation of anhydrite occurrences and features support both primary and secondary formations. The nodular to chicken-wire anhydrite formed under synsedimentary sabkha conditions, whereas anhydrite cements occurred during the late stages of diagenesis (shallow burial stage). Massive to bedded anhydrite could have been formed under subaqueous conditions or originated by coalescing and continued growth of anhydrite nodules in the sabkha zone. Anhydrite fabrics impose a significant control on the reservoir quality of the Kangan carbonates at the South Pars Gas Field. Thick massive and bedded anhydrite could have been formed as an intraformational seals and anhydrite cements occluded pore spaces and reduced the poroperm values. The sequence stratigraphic analysis revealed two depositional sequences in the studied intervals, which are composed of TST and HST. Investigation of anhydrite throughout depositional sequences indicates a change in the content and style of anhydrite texture. Anhydrite content (volume) decreases upward through transgressive system tract (sea-level rise) whereas, it enhances during highstand system tract (sea-level fall). Pervasive and poikilotopic anhydrite cements together with replacement by anhydrite are prevalent features during transgressive and early highstand system tract. At the late HST, with a progradational stacking pattern, anhydrite value increases and felted, radial, equant, crystalline and mosaic texture are the most common anhydrite fabrics. Sequence boundaries that indicate maximum sea level fall and exposure of successions are marked by the broad anhydrite deposits with massive to bedded and chicken-wire structures and various textures that located in late HST package. There is an unambiguous relationship between the microfacies associations, the evaporite textures, and the sea-level fluctuations. This relationship could lead to a predictable pattern that can be of use as a general guide for the sequence stratigraphic interpretations in the area.  相似文献   

Filling the gap: A 60 ky record of mixed carbonate-siliciclastic turbidite deposition from the Great Barrier Reef     

《Marine and Petroleum Geology》2014

Late Pleistocene to Holocene margin sedimentation on the Great Barrier Reef, a mixed carbonate-siliciclastic margin, has been explained by a transgressive shedding model. This model has challenged widely accepted sequence stratigraphic models in terms of the timing and type of sediment (i.e. carbonate vs. siliciclastic) deposited during sea-level oscillations. However, this model documents only hemipelagic sedimentation and the contribution of coarse-grained turbidite deposition, and the role of submarine canyons in this process, remain elusive on this archetypal margin. Here we present a new model of turbidite deposition for the last 60 ky in the north-eastern Australia margin. Using high-resolution bathymetry, 58 new and existing radiometric ages, and the composition of 81 turbidites from 15 piston cores, we found that the spatial and temporal variation of turbidites is controlled by the relationship between sea-level change and the variable physiography along the margin. Siliciclastic and mixed carbonate-siliciclastic turbidites were linked to canyons indenting the shelf-break and the well-developed shelf-edge reef barriers that stored sediment behind them. Turbidite deposition was sustained while the sea-level position allowed the connection and sediment bypassing through the inter-reef passages and canyons. Carbonate turbidites dominated in regions with more open conditions at the outer-shelf and where slope-confined canyons dominated or where canyons are generally less abundant. The turn-on and maintenance of carbonate production during sea-level fluctuations also influenced the timing of carbonate turbidite deposition. We show that a fundamental understanding of the variable physiography inherent to mixed carbonate-siliciclastic margins is essential to accurately interpret deep-water, coarse-grained deposition within a sequence stratigraphic context.  相似文献   

中国大陆及边邻地区6 级以上地震序列的最大余震统计特征     

任雪梅  谭俊林  马禾青  曾宪伟 《中国地震》2013,29(4):480-488

依据1966 年以来中国大陆及边邻地区记录相对完备的6 级以上地震序列资料,统计研究了地震的破裂类型和不同破裂类型下余震序列特征等,得到了不同破裂类型下不同余震序列比例和优势分布、主震震级与最大余震震级差的经验关系。主震与最大余震的震级关系线性较好,得到的经验公式可以为中国大陆及边邻地区同类地震的最大余震震级判定提供参考;最大余震发生在主震后10 天内的比例为43. 8% ～ 81. 8% ,正断型和走滑型中的孤立型的最大余震发生在主震后10 天内的比例高达80% 。  相似文献   

新疆尼勒克、巩留交界M_S6.0地震前部分地震学异常及序列特征     

聂晓红  高朝军  史新娣 《内陆地震》2012,26(3):193-202

对尼勒克、巩留交界MS6.0地震序列特征、震源机制以及震前震中周围地区地震活动图像异常特征等进行了分析。结果认为,本次地震序列为主-余型,震源机制为逆断型,发震构造为阿吾拉勒山南缘断裂。震前中期阶段存在4级地震空区、4级地震条带、小震群累积月频次和地震活动性参数等异常;短期异常出现了3级地震空区、3级地震平静、地震窗和地震波振幅比等异常。此次地震前出现的部分异常与2007年特克斯5.9级地震前的地震活动异常图像具有类似特征。  相似文献