Onshore-offshore gradient in reductive early diagenesis in coastal marine sediments of the Ria de Vigo, Northwest Iberian Peninsula     

K.J. Mohamed  D. ReyB. Rubio  M.J. DekkersA.P. Roberts  F. Vilas 《Continental Shelf Research》2011,31(5):433-447

Early diagenetic modification of magnetic properties is an important process in marine sediments, but temporal and spatial variability of diagenetic processes have rarely been reported for recent coastal sediments. The magnetic properties of sediments from the Ria de Vigo (NW Spain) define a marked three-part zonation with depth. The uppermost zone is magnetically dominated by (titano-)magnetite. In the intermediate zone, rapid down-core dissolution of (titano-)magnetite increases the relative influence of high-coercivity magnetic minerals, which react more slowly during reductive dissolution than (titano-)magnetite. This zone is characterized by the ubiquitous occurrence of framboidal iron sulphides. Pyrite is the dominant iron sulphide, but framboidal ferrimagnetic greigite is also frequently observed in association with pyrite. The lowermost zone is characterized by an almost complete depletion of magnetic minerals associated with progressive reduction of detrital iron oxides with depth. This zonation is controlled by organic matter diagenesis, which varies with water depth and wave-induced sediment resuspension and organic matter reoxidation in the water column. This leads to a shallowing and thinning of each zone with more intense reductive diagenesis toward the interior of the ria. Such a zonation seems to be a common feature in shallow water marine environments. If preserved, the described zonation and its spatial variability provide a potential tool for detecting estuarine-like environments in the geological record. Magnetic detection of current or past reductive conditions also has important implications for assessing paleoenvironmental proxies that are sensitive to diagenetic redox state.  相似文献   

全球地震早期预警研究综述   总被引：6，自引：2，他引：4       下载免费PDF全文

赵冰  刘希强 《地震工程学报》2011,33(4):392-402

近年来地震预警技术在国际上得到迅速的发展,并有成功预警且收到减灾实效的先例.本文系统介绍了地震早期预警的方法,包括波前探测、P波应用、现地预警和区域预警;介绍了地震早期预警系统在墨西哥、日本、土耳其、中国台湾和罗马尼亚等国家和地区的应用情况.还对地震预警中目前存在的问题和挑战以及远景进行了分析.  相似文献   

适用于低延时实时数据传输的地震数据压缩方法     

陈阳  薛兵  朱小毅  李江  林湛  张志强 《地震地磁观测与研究》2011,32(6):127-132

随着数字地震台站数量的增加、数据传输手段的多样化以及地震预警系统的发展,对地震数据实现有效的实时压缩对数据传输显得十分重要.本文提出一种支持低时间延迟(数据传输间隔小于1 s)数据传输要求的实时数据压缩算法.通过理论估算和实际地震数据检验,该方法高效、易实现,适用于地震预警等领域.  相似文献   

关于“辽宁北票兴隆沟火山岩的野外产状、岩石成因及地质意义”一文的辩正   总被引：1，自引：0，他引：1  

邵济安  杨蔚 《地质学报》2011,85(3):379-382

本文针对"辽宁北票兴隆沟火山岩的野外产状、岩石成因及地质意义"一文对笔者的质疑,阐述了对北票下侏罗统兴隆沟组开展地质调查的经过.结合质疑的问题,从野外地质观察和同位素年代学两个方面展开讨论,并且根据新获得的火山岩202Ma的Ar-Ar年龄,重申辽西北票兴隆沟组的时代属于早侏罗世的结论.  相似文献   

Late Albian (Early Cretaceous) ammonites from the Provincial Formation of central Cuba     

Ricardo Barragán  Reinaldo Rojas-ConsuegraOttilia Szives 《Cretaceous Research》2011,32(4):447-455

A late Albian ammonite assemblage from the Provincial Formation of Villa Clara Province, Cuba is described. The Provincial Formation is a lithostratigraphic unit of Albian-Cenomanian age extensively exposed in central Cuba and formed within a part of the Caribbean Tethys that was volcanic during the Cretaceous. The formation is mainly composed of calcareous, terrigenous marine, and volcano-sedimentary deposits characterized by a series of micritic limestones intercalated with marls, sandstones, calcareous conglomerates, ash, and tuffaceous material. A rich assemblage of ammonites recovered from the calcareous biomicrites and marls is of late Albian (Stoliczkaia dispar Zone, Mortoniceras rostratum Subzone) age. The ammonite fauna shows a strong Tethyan affinity, and only a single hoplitid ammonite species was recorded. Although scarce, the first Cuban report of this and other boreal ammonite species now allows precise correlations to be made between Cuba and Albian sediments elsewhere in the world.  相似文献   

江西南部武夷群及其地质时代   总被引：3，自引：0，他引：3  

巫建华  项媛馨  刘帅 《地层学杂志》2011,(2):200-208

江西南部三百山、蔡坊、版石、岩背等火山盆地由长英质火山岩组成,岩石组合与北武夷地区的武夷群一致,可归人武夷群,并可进一步划分出双峰岭和鹅湖岭两个组.错石SHRIMP U-Pb测年结果表明,三百山盆地粗面岩的年龄为142.0±1.0Ma,蔡坊盆地流纹岩的年龄为131.4±1.3Ma,版石盆地围东一带流纹质凝灰岩的年龄为1...  相似文献   

New Albian macro- and palynoflora from the Negev (Israel) with description of a new gymnosperm morphotaxon     

Valentin Krassilov  Eckart Schrank 《Cretaceous Research》2011,32(1):13-29

New plant macrofossil localities are found in the middle-upper part of the Albian Upper Hatira Formation of Makhtesh Qatan, an erosion crater in the northern Negev. These are so far the only outcrop localities in the Negev containing plant compressions and well-preserved sporomorphs. Their age assignments are controlled by the ammonite Knemiceras records below and above the plant-bearing sequence in the adjacent Makhtesh Hatira. The macrofossil assemblages are strikingly different in the sandy fluvial and shaly lacustrine facies, the former being dominated by Araucaria, Athrotaxopsis, Brachyphyllum and pinnatifid Sapindopsis, comparable at the plant assemblage and leaf morphological levels to the early to early late Albian assemblage of the North American Potomac flora. The lacustrine shale macrofossil assemblages appear archaic on account of their diverse pteridophyte component and sparse angiosperm remains. A new supposedly gnetophytic genus and species Qataniaria noae Krassilov, gen. et sp. nov. is dominant in the shale horizon. The sporomorph assemblages are strongly dominated by psilate trilete spores (87-93%). In the absence of elaterate forms, the angiosperm pollen Afropollis jardinus, Pennipollis, Tricolpites spp. and Walkeripollis sp. is consistent with the early Albian age. The abundance and diversity of conifers and the prominence of the fern bog assemblage suggest a relatively humid phase of the regional Albian climates.  相似文献   

雪峰山早中生代构造演化:构造学和年代学分析木   总被引：1，自引：0，他引：1       下载免费PDF全文

褚杨  林伟  Michel Faure  王清晨 《地质科学》2011,46(1):146-160

雪峰山主体地处湖南省境内,位于华南板块的中心区域,是一条典型的陆内造山带.通过详细的野外地质观察,我们将其分为3个构造单元:西部外区,主要以大型箱状褶皱为主;中部区,与西部区以主逆冲断层相分隔,劈理发育呈扇状,是雪峰山构造带的核心区域,也是变质级别最深、变形最强的区域;东部区,变形集中在脆韧性区域之上,以极性北西构造为...  相似文献   

河南省太原组沉积时期岩相古地理特征   总被引：10，自引：1，他引：9  

宋慧波  胡斌  张璐  刘顺喜  牛永斌 《沉积学报》2011,29(5):876-888

河南省早二叠世太原组沉积区位于华北盆地南部北秦岭褶皱带栾川—固始深断裂以北地区,当时的沉积盆地受华北地块西隆东倾的构造古地理控制,是晚古生代华北陆表海盆地或碳酸盐岩台地沉积的一部分,发育了一套以碳酸盐岩为主夹碎屑岩和煤为特色的陆表海沉积。太原组岩性以灰—深灰色薄—中厚层状生物屑灰岩为主,夹薄—中厚层状的泥岩、泥灰岩、细...  相似文献   

青藏高原东南缘腾冲早白垩世岩浆岩锆石SHRIMPU-Pb定年和Lu-Hf同位素组成及其构造意义   总被引：17，自引：16，他引：1  

戚学祥  朱路华  胡兆初  李志群 《岩石学报》2011,27(11):3409-3421

早白垩世花岗闪长岩和石英二长岩是腾冲地块内重要的岩石类型,以舍角闪石为特征,其高钠低钾和偏铝质性质展示其Ⅰ型花岗岩的属性.锆石SHRIMP U-Pb定年结果表明花岗闪长岩和石英二长岩分别侵位于122±1.3Ma和125±1.3Ma,其锆石εHf(t)值分别为-9.6～-4.8(平均-6.7±0.7)和-7.8～-4.7(平均-6.3±0.6),对应的单阶段模式年龄为979～1190Ma和975～1113Ma.在εHf(t)-U-Pb年龄图解上所有样品都落在球粒陨石线和下地壳线之间区域,以及较高的Al2O3含量和Th/Hf比值揭示其壳源特征,但锆石εHf(t)值变化范围较大,其绝对值远小于完全由壳源物质部分熔融形成的岩浆岩,以及高Th/Yb、低Ba/La和Yb/Hf比值说明除壳源外,还有幔源组分的加入.岩石富钠贫钾、在微量元素蛛网图和稀土配分曲线图上展示出LILE(Rb、Sr、K和Ba)相对原始地幔强烈富集,Ba、Nb、Ta、Sr、P、Ti和Eu负异常,以及微量元素和常量组分判别图解都显示其形成于俯冲碰撞的构造环境.腾冲早白垩世岩浆岩的形成时代、锆石Lu/Hf同位素组成及其对应的单阶段模式年龄、微量元素特征与中拉萨和拉萨地块东缘的火成岩非常相似,暗示腾冲早白垩世岩浆岩带是中拉萨岩浆岩带的东南延伸部分,是对中特提斯洋壳沿班公湖-怒江缝合带向拉萨-腾冲地块下俯冲碰撞的响应.  相似文献