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   总被引：5，自引：0，他引：5       下载免费PDF全文

刘招君  孙平昌  贾建亮  柳蓉  孟庆涛 《地学前缘》2011,18(4):171-180

陆相盆地深水环境是油页岩、暗色泥岩沉积区域,深水层序研究是勘探开发此类能源的基础工作.但深水沉积多为暗色泥岩沉积,很难准确划分多级层序.在松辽盆地3口全取心井、测井及测试资料分析基础上,发现在深水区域,油页岩层或生物富集层底界面、TOC、含油率、生烃潜量、氢指数、氢/氧指数突然增高点及沉积物密度突变小处、伽马测井坎值均...  相似文献   

Morphology and Molecular Identification of Ulva Forming Green Tides in Qingdao, China     

KONG Fanna  MAO Yunxiang  CUI Fujun  ZHANG Xingkui  GAO Zhen 《青岛海洋大学学报(英文版)》2011,(1):73-79

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Morphology and molecular identification of Ulva forming green tides in Qingdao, China     

Fanna Kong  Yunxiang Mao  Fujun Cui  Xingkui Zhang  Zhen Gao 《中国海洋大学学报(英文版)》2011,10(1):73-79

Green tides are caused by the proliferation of chlorophytes under suitable hydrographic conditions.These blooms lead to environmental degradation and negatively impact the waters and seagrass beds,as well as fishing and other recreational activities in the bay.A comprehensive ecological understanding of the bloom dynamics,including the origin and persistence,is needed to foster management decisions.The algae in the great majority of green tide blooms usually belong to two genera of Ulvophyceae,Ulva and Enteromorpha.Ulva has been observed more often in recent years.In China,green tides occurred for the first time in the middle area of the Yellow Sea in 2007,and a large-scale algae blooming broke out in the middle and southern areas of the Yellow Sea in late May 2008.We identified them as Ulva prolifera by comparative analysis of the rDNA internal transcribed spacer 1 (ITS1),5.8S and ITS2 sequences in combination with microscopic observation.Morphological differences were found between the free-floating algae and the attached thalli.Various reproduction patterns of the free-floating algae include sexual,asexual and vegetative propagations,which played important roles in the long-term green tide persistence in China.The ITS sequences of the blooming algae were identical to those of the samples from the Lianyungang sea area but were different from the attached samples from the Qingdao sea area.The results infer that the blooms are originated from other sea areas rather than from the local attached populations.  相似文献   

A geophysical transect of the Adélie Margin,East Antarctica     

Jacques Wannesson  Monique Pelras  Bernard Petitperrin  Martine Perret  Jacques Segoufin 《Marine and Petroleum Geology》1985,2(3):192-200

In 1982, a geophysical survey of the Antarctic margin, including multichannel seismic, gravity, magnetic and bathymetric surveying, was carried out off Adélie Coast-Wilkes Land and in the eastern Ross Sea. Of the 5000 km of lines recorded, 3000 km were in the Adélie Coast area. Lines ATC 101–102, approximately following meridian 138°E, show the first complete transect of the Adélie Coast margin from the Southeast Indian abyssal plain at DSDP Site 269 to the continental shelf. These lines reveal a thick sedimentary series divided into three main acoustic units by two major unconformities considered to be Upper Eocene (42 Ma) and late Oligocene (25 Ma). Oceanic or continental basement can be traced under the whole area, and the ocean-continent boundary clearly lies beneath the lower continental slope. A deep, high-amplitude, low-frequency horizon, extending under the oceanic basement for over 300 km of line, is considered to be the Moho. Our interpretation supports a recent revision be Cande and Mutter proposing an early Upper Cretaceous opening between Australia and East Antarctica.  相似文献   

The depositional architecture and facies variability of shelf deltas in the Eocene Battfjellet Formation,Nathorst Land,Spitsbergen     

Sten‐Andreas Grundvåg  William Helland‐Hansen  Erik P. Johannessen  Andreas H. Olsen  Stig A. K. Stene 《Sedimentology》2014,61(7):2172-2204

Deltas are commonly classified according to their plan‐view morphology as either river‐dominated, tide‐dominated or wave‐dominated. However, most deltas form under the mixed influence of these processes, commonly with laterally varying process regimes. It has also become clear that there is a mismatch between the plan‐view morphology and internal facies composition in some deltas. Combined outcrop and subsurface data from the Eocene Battfjellet Formation, Spitsbergen, provide an example of ancient shelf deltas that formed under mixed influence. Internally, these shelf deltas are characterized by wave‐dominated facies that are normally associated with strike‐extensive, nearly linear shoreline sandstones. However, the formation comprises partially overlapping sandstone bodies of limited lateral extent (<20 km in any direction). This stacking pattern is attributed to frequent autogenic lobe switching that caused localized and rapid transgressions. Such processes typify fluvial‐dominated deltas and occur less commonly in wave‐dominated ones. Thus, there is an apparent mismatch between inferred plan‐view morphology and internal facies composition. It is argued that the Battfjellet deltas were flood‐dominated and prograded mainly during periods of high fluvial discharge. However, reworking of the fluvial‐flood facies by fair‐weather and storm waves, as well as longshore currents, resulted in a wave‐dominated facies character. Delta lobes undergoing auto‐retreat were particularly prone to reworking by basinal processes, including tidal currents. It is suggested that repeated delta progradation from inner shelf settings towards the outer shelf and shelf edge was aided by high sediment supply rather than relative falls in sea‐level as previously suggested. This interpretation is supported by: (i) the lack of major facies dislocations and extensive sub‐aerial unconformities; and (ii) an overall relative rise in sea‐level as evidenced by an overall low‐angle (0·8 to 1·2°) ascending shoreline trajectory. The latter results from the combined effect of basin subsidence, eustatic highstand and sediment compaction.  相似文献   

Rapid texture mapping from image sequences for building geometry model     

Zhang Zuxun  Wu Jun  Zhang Jianqing 《地球空间信息科学学报》2013,16(3):8-15

An effective approach, mapping the texture for building model based on the digital photogrammetric theory, is proposed. The easily-acquired image sequences from digital video camera on helicopter are used as texture resource, and the correspondence between the space edge in building geometry model and its line feature in image sequences is determined semiautomatically. The experimental results in production of three-dimensional data for car navigation show us an attractive future both in efficiency and effect.  相似文献   

Quantitative Biostratigraphic Analysis upon the Upper Cretaceous in Tethyan Himalaya     

LI Guangwei  ZENG Jun 《《地质学报》英文版》2013,87(4):926-935

Biostratigraphic analysis is an essential element for understanding global tectonics and the evolution of life on Earth. Quantitative analysis of sedimentary sequences provides the precise age constraints on timing of significant events in Earth’s history. This paper presents results from quantitative stratigraphic analysis of Upper Cretaceous Tethyan Himalayan sequences. This analysis resulted in a new composite stratigraphic section for the Cretaceous strata of Tibet (TIBETKCS). The eight Upper Cretaceous sections were analyzed in this study and 12 planktonic foraminifera zones were recognized based on available data. Quantitative measurements were made using a Graphic Correlation with Graphcor 3.0 software and correlated to the world standard Cretaceous Composite Section (MIDKCS). The sections were also examined using Constrained Optimization software by CONOP9. Level Penalty was applied as the rule to measure misfit among automatically correlated sections. The new TIBETKCS correlates well with planktonic foraminifera ages from previous work in southern Tibet. A fitting equation of y=?0.19x+305 with a correlation coefficient of 0.94 was obtained from this work. The ages of the first and last appearances of 64 planktonic foraminifera can be calculated with this equation with ± 0.3 Ma precision. This level of precision is approximately 10 times higher than age determinations with traditional methods. Two extinction events were resolved within this analysis at ~93.5 Ma and ~85.5 Ma corresponding to the Ocean Anoxic Events at Cenomanian–Turonian and Coniacian–Santonian boundaries respectively.  相似文献   

基于地层层序表集的三维地层建模方法研究     

陆文哲  陶海冰  朱益军  刘干斌 《岩土力学》2013,34(2):585-592

钻孔样本间因存在地层层序不一致而导致无法确定建模时各地层拓扑关系,是采用钻孔数据建立三维地质模型的难点。拟通过下述方法解决这一难点：在已知的主地层层序表情况下,由主地层层序表结合钻孔信息推测出其他地层层序表,建立地层层序表集,再通过运用空间分析的手段来确定钻孔样本与各张地层层序表的归属关系,采用最大数目地层连接法来自动确定两个地层层序表间相互连接关系,并得到合并表;然后结合这种连接法,将全部地层层序表合并为一张最终地层层序表,从而确定所有地层拓扑关系;所有钻孔数据按照最终表进行标准化,之后运用表面建模方法进行三维地层建模。在诸永高速公路K120+030～K120+300段滑坡区域的三维地层建模中,运用该方法验证了其有效性。  相似文献   

2014年新疆于田MS7.3地震序列特征及早期趋势判断     

宋春燕  张琳琳  聂晓红  夏爱国  魏芸芸 《地震研究》2014,37(4)

介绍了2014年2月12日新疆于田MS7.3地震的基本参数、发震构造和地震序列特征,并与2008年于田MS7.3地震序列特征进行对比分析.结果显示,2014年于田MS7.3地震有MS5.4直接前震,序列强余震频次低、余震衰减较快,目前最大余震震级为MS5.7;通过分析历史地震序列类型、计算于田单台序列的h值、6值、主震释放的能量与序列能量的比值等参数,初步判断于田MS7.3地震序列为“前震—主震—余震型”.  相似文献   

龙门山南段构造变形及应力序列   总被引：2，自引：2，他引：0  

宋春彦  刘顺  何利 《大地构造与成矿学》2009,33(3)

2008年5月12日的汶川大地震表明龙门山断裂带仍然是一个构造活动带,为达到防震减灾的目的,对龙门山进行深入研究显得非常必要。作者通过龙门山南段的怀远和雅安两条实测构造地质剖面,应用传统的构造解析法,结合构造带的分带讨论思想,对野外实测的褶皱、节理和断层等构造变形要素进行综合分析,确定出各构造带的变形和应力序列。中央断裂带构造变形次数达10次以上,其中以NW-SE向逆冲最多,部分为左旋逆冲或右旋逆冲。滑覆体构造变形序列达5次左右。前山断裂带的构造变形序列较少,约5次以上。  相似文献