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系统的探讨了区内白垩纪地层的划分与沉积相特征,深入研究了陆相地层的层序发育特征。指出,无论冲积扇、河流、三角洲或湖泊沉积的陆相地层层序均受地层基准面控制。地层基准面穿越旋回控制着陆相环境重大层序分布。根据不同时间间隔的基准面穿越旋回序次,将陆相层序划分为盆地充填层序、构造层序、层序、亚层序及小层序五个级别。每个层序根据基准面波动可划分为基准面上升沉积体系域和基准面下降沉积体系域,并可根据亚层序组的叠置特征进一步细分。根据上述陆相地层层序划分原理,作者将研究区白垩纪陆相地层划分为三个构造层序,并初步将葛村组划分为五个、浦口组四个、赤山组三个和泰州组三个沉积层序。 相似文献
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试论陆相火山岩区火山地层单位与划分──关于火山岩区填图单元划分的讨论 总被引:1,自引:0,他引:1
火山活动具多旋回性,一个火山活动旋回的岩浆作用产物及其形成的火山构造形迹具时空分布协调性,同一旋回的火山构造在空间上呈串珠状或并列式展布,不同旋回的火山构造在空间上呈叠置式展布;火山喷发类型与火山岩相具一致性,岩相及相序是推演古火山演化历史、恢复古火山机构的主要依据,亦是组成火山地层并且成因意义的单元;不同旋回火山机构内的火山地层层序的综合、叠置是建立区域火山地层层序的基础;火山构造是火山岩区地质构造的主要内容,以区域构造、火山构造、火山岩浆作用产物的岩相为内容的火山岩相构造图是揭示火山岩区地质构造特征的综合性图件;环形火山构造叠置与区域线形构造交织分布组成线─环形境构造格局.是火山岩区所特有的构造面貌,在火山地质图上应得到充分的体现;。根据上述认识,对陆相火山岩区作为火山地层填图单元的岩石地层单位群─组─段─层划分提出了方案,建议用旋回─组─岩相─层(即火山构造─组─岩相─层)四级作为火山地层划分单位和填图单元,其中旋回火山构造一致,组与火山机构演化阶段一致,岩相与火山喷发类型一致,层为岩相内容的补充。据此填制的火山地质图才能真正成为反映火山岩浆作用及其产物的特色和具普遍意义的图件。 相似文献
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香港海沙资源的勘探开发与管理 总被引:1,自引:0,他引:1
海沙开采已成为仅次于油气开采的世界第二重要海洋开采业。1980年代以来,香港政府投资1.7×108港元为寻找海岸围垦填料进行了一系列的海沙勘探活动,在1828km2香港水域发现22个地点海沙资源储量7.4×108m3,其中9个地点4.2×108m3储量因覆盖层较厚或污染严重或海区环境特别敏感等原因被暂时搁置。1990~2002年共开采海沙2.7×108m3,为形成2100hm2新土地的多项围垦工程提供了约一半的填料。基于地球物理勘探和钻探资料建立了香港海域第四纪层序和海沙产状地质模型,发现和证实了含气沉积物地震剖面的声波浑浊现象。香港政府对海沙资源进行统一勘探和统一管理,强调海沙开采的环境和生态影响评估,利用废弃的海床挖沙坑回填倾废的非污染海泥和受污染海泥。我国内地海沙勘探管理可以从中取得借鉴。 相似文献
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二叠纪—三叠纪之交的环境恶化事件不但导致了生物大绝灭,而且造成了自然界正常的碳循环崩溃。为了研究三叠纪早期生物复苏过程中的环境特征、碳氧同位素演化上的地层学意义,对巢湖平顶山西坡剖面下三叠统碳酸盐岩取样分析。研究结果表明,巢湖平顶山西坡剖面早三叠世碳氧同位素地层曲线与已知的平顶山北坡剖面碳氧同位素地层曲线相似。δ13C值在Induan阶、Olenekian阶底部首先表现为大幅度负漂,随后呈上升趋势。δ18O值除了表现出1Ma的周期性波动之外,与δ13C低值区对应处也具负偏趋势。δ13C、δ18O值的演化趋势反映了早三叠世海洋环境恶化、生物复苏十分缓慢。 相似文献
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Callaghan TV Tweedie CE Akerman J Andrews C Bergstedt J Butler MG Christensen TR Cooley D Dahlberg U Danby RK Daniëls FJ de Molenaar JG Dick J Mortensen CE Ebert-May D Emanuelsson U Eriksson H Hedenås H Henry H R G Hik DS Hobbie JE Jantze EJ Jaspers C Johansson C Johansson M Johnson DR Johnstone JF Jonasson C Kennedy C Kenney AJ Keuper F Koh S Krebs CJ Lantuit H Lara MJ Lin D Lougheed VL Madsen J Matveyeva N Mcewen DC Myers-Smith IH Narozhniy YK Olsson H Pohjola VA Price LW Rigét F Rundqvist S 《Ambio》2011,40(6):705-716
Understanding the responses of tundra systems to global change has global implications. Most tundra regions lack sustained environmental monitoring and one of the only ways to document multi-decadal change is to resample historic research sites. The International Polar Year (IPY) provided a unique opportunity for such research through the Back to the Future (BTF) project (IPY project #512). This article synthesizes the results from 13 papers within this Ambio Special Issue. Abiotic changes include glacial recession in the Altai Mountains, Russia; increased snow depth and hardness, permafrost warming, and increased growing season length in sub-arctic Sweden; drying of ponds in Greenland; increased nutrient availability in Alaskan tundra ponds, and warming at most locations studied. Biotic changes ranged from relatively minor plant community change at two sites in Greenland to moderate change in the Yukon, and to dramatic increases in shrub and tree density on Herschel Island, and in subarctic Sweden. The population of geese tripled at one site in northeast Greenland where biomass in non-grazed plots doubled. A model parameterized using results from a BTF study forecasts substantial declines in all snowbeds and increases in shrub tundra on Niwot Ridge, Colorado over the next century. In general, results support and provide improved capacities for validating experimental manipulation, remote sensing, and modeling studies. 相似文献
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论浙东南磨石山群祝村组的解体 总被引:1,自引:0,他引:1
对浙东南磨石山群祝村组层型———丽水祝村剖面及其附近进一步地质调查时发现祝村组“下伏”的九里坪组为一个英安玢岩侵出体。祝村组建组的基础不存在。祝村组下部英安质熔结凝灰岩和上部流纹岩Nd同位素测定结果 :εNd(t)值和T2DM值分别为 - 9.6、- 7.2和1.70Ga、1.5 1Ga ,表明它们物质来源不同 ,属于不同火山旋回的产物。根据地层层序、岩石组合及与区域磨石山群地层对比 ,祝村组应解体为西山头组、茶湾组和九里坪组。祝村组一名不宜继续使用 相似文献
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Polar and alpine environments are changing rapidly due to increases in temperature, which are amplified in the Arctic, as
well as changes in many local factors. The impacts on ecosystems and their function have potential consequences for local
residents and the global community. Tundra areas are vast and diverse, and the knowledge of geographical variation in environmental
and ecosystem change is limited to relatively few locations, or to remote sensing approaches that are limited mostly to the
past few decades. The International Polar Year, IPY, provided a context, stimulus and timely opportunities for re-visiting
old research sites and data sets to collate data on past changes, to pass knowledge from old to new generations of researchers
and to document environmental characteristics of sites to facilitate detection and attribution of future changes. Consequently,
the project “Retrospective and Prospective Vegetation Change in the Polar Regions: Back to the Future,” BTF, was proposed
and endorsed as an IPY activity (project #512). With national funding support, teams of researchers re-visited former sites
and data sets throughout the Arctic and some alpine regions. These efforts have amounted to a gamut of “BTF” studies that
are collectively geographically expansive and disciplinary diverse. A selection of these studies are introduced and presented
in the current issue together with a brief synthesis of their findings. 相似文献