关于《中国扬子区兰多维列统特列奇阶及其与英国的对比》一书若干问题的商榷     

林宝玉  李明  黄莫  邓丽婷 《地质论评》2021,67(4):67040849-67040868

《中国扬子区兰多维列统特列奇阶及其与英国的对比》一书(陈旭和戎嘉余,1996)有以下结论:(1)将回星哨组、茅山组、西坑组等的层位归属于特列奇阶上部;(2)将回星哨组、茅山组及其相当地层与英国特列奇阶对比;(3)将扬子区特列奇阶的顶界置于回星哨组、茅山组及其相当地层之顶;(4)将回星哨组、茅山组、西坑组等地层资料编制的古地理图称为特列奇期晚期古地理图;(5)将回星哨组、茅山组、西坑组等地层与上覆中泥盆统—中二叠统之间的不整合面代表的上升运动,称为"特列奇期的扬子上升"。笔者等依据多年对扬子地台志留纪地层剖面的实地考察和近数十年来扬子区坟头组中—上部、茅山组、回星哨组、小溪峪组、西坑组等地层中文洛克世、拉德洛世、普里多利世早期古生物化石的发现,认为:(1)回星哨组、小溪峪组、茅山组、西坑组等的层位是文洛克统—普里多利统;(2)回星哨组、小溪峪组等大致与英国的文洛克统—普里多利统对比;(3)回星哨组、小溪峪组、茅山组的顶界是文洛克统—普里多利统剥蚀后残留的层位随地而异的顶界;(4)根据回星哨组、西坑组、茅山组等地层资料编制的古地理图应是文洛克世—普里多利世古地理图;(5)"扬子地台整个上升"(Huang T K,1945)的时代是志留纪末期,没有"特列奇期的扬子上升"。特提出商榷。上述这些地层时代的解决,对扬子区志留系4统层序的建立具有重要意义,而且也为中国扬子区与英国命名剖面志留系的对比以及中国南方早古生代加里东运动最后一幕时代的再次确定提供了地层学和古生物方面的依据。  相似文献   

Carbon and strontium isotope stratigraphy of the Upper Cretaceous (Cenomanian-Campanian) shallow-water carbonates of southern Italy: Chronostratigraphic calibration of larger foraminifera biostratigraphy     

《Cretaceous Research》2015

Shallow-water carbonates are invaluable archives of past global change. They hold the record of how neritic biologic communities reacted to palaeoenvironmental changes. However, attempts to decipher these geological archives are often severely hampered by the low stratigraphic resolution attained by biostratigraphy. This is particularly the case for the Upper Cretaceous carbonate platforms of the central Tethyan realm: their biostratigraphy suffers from very low resolution and poor correlation with the standard biochronologic scales based on ammonites, planktic foraminifers and calcareous nannoplankton.In this paper we show how this problem can be tackled by integrating biostratigraphy with isotope stratigraphy. We present a detailed record of the benthic foraminiferal biostratigraphy and carbon and strontium isotope stratigraphy of three upper Cenomanian-middle Campanian sections belonging to the Apennine Carbonate Platform of southern Italy. For the upper Cenomanian-Turonian interval, the carbon isotope curves of the studied sections are easily correlated to the reference curve of the English Chalk. The correlation is facilitated by the matching of the prominent positive excursion corresponding to the Oceanic Anoxic Event 2. For the Coniacian-middle Campanian interval, the correlation is mainly based on strontium isotope stratigraphy. We use the ⁸⁷Sr/⁸⁶Sr ratios of the low-Mg calcite of well preserved rudist shells to obtain accurate chronostratigraphic ages for many levels of the three studied sections. The ages obtained by Sr isotope stratigraphy are then used to better constrain the matching of the carbon isotope curves.From the high-resolution chronostratigraphic age-model stablished by isotope stratigraphy, we derive the chronostratigraphic calibration of benthic foraminiferal biostratigraphic events. For the first time the benthic foraminiferal biozones of the Apennine Carbonate Platform can be accurately correlated to the standard ammonite biozonation. This result is of great relevance because the biostratigraphic schemes of other carbonate platforms in the central and southern Tethyan realm are largely based on the same biostratigraphic events.  相似文献   

四川省盐源玻璃村特大型玄武岩古滑坡复活机制     

何坤  胡卸文  马国涛  刘波  梅雪峰  王蛟  杨群 《岩土力学》2020,41(10):3443-3455

受前期14 d持续累计350.6 mm降雨影响,2018年7月19日盐源玻璃村一巨型玄武岩古滑坡体发生大规模复活,复活体积为1 390×104 m3,损坏房屋186间,造成重大经济损失。基于现场调查、无人机航测、钻探揭露、物理力学试验及数值模拟分析,在查明滑坡体地质结构、失稳特征基础上,对其影响因素及复活机制进行了探讨。研究结果表明,破碎岩土体及地形地貌是滑坡复活的孕灾基础,持续降雨及其引起的地下水位升高是滑坡复活的诱发因素。复活滑坡可分为主滑区和侧滑区两种破坏模式不同的区域。降雨作用下滑坡体内渗流场明显变化,孔隙水压力增大,导致7月13日古滑坡体开始发生变形,稳定性系数逐渐降低。受微地貌约束,主滑区具有多级、多次失稳,渐进破坏的特点。侧滑区斜坡前缘临空条件受坡脚主滑坡控制,在主滑坡运动过程中,侧滑区坡体位移量、最大剪切应变增量逐渐增大,塑性区扩展,破坏过程表现出与主滑坡一定的关联性和滞后性。分析表明,受地下水长期影响,滑带土体强度逐渐削弱,降雨导致坡体渗流作用加剧,抗剪强度降低,从而诱发滑坡复活。  相似文献   

地理信息公共服务平台建设的有效驱动     

苗前军 《测绘软科学研究》2010,(1):6-11

通过研究我国地理信息公共服务平台建设的驱动现状及其相关问题,分析了地理信息公共服务平台的层次结构以及在空间信息技术发展中的定位,基于地理信息公共服务平台的试点工程应用示范建设的经验,阐述了地理信息公共服务平台建设的有效驱动问题。针对我国当前地理信息公共服务平台建设中的瓶颈问题,提出了走以不同行业与部门协同共建的方式来有效驱动地理信息公共服务平台建设的路径。  相似文献   

Lower Carboniferous (Dinantian) stratigraphy and structure of the Walterstown-Kentstown area,Co. Meath,Ireland     

Neil A. H. Pickard  Gareth Li. Jones  John G. Rees  Ian D. Somerville  Peter Strogen 《Geological Journal》1992,27(1):35-58

Stratigraphic units are defined and described for the Lower Carboniferous succession in the Walterstown-Kentstown area of Co. Meath, Ireland. A complete (unexposed) Courceyan succession from the terrestrial red bed facies of the Baronstown Formation to the Moathill Formation of the Navan Group has been penetrated in several boreholes. Although the lower part of the sequence is comparable with the Courceyan succession at Navan and Slane, the middle part of the sequence differs markedly in the Walterstown-Kentstown area and two new members, the Proudstown and Walterstown Members, are defined in the upper part of the Meath Formation. Syndepositional faulting was initiated during the Courceyan, probably in latest Pseudopolygnathus multistriatus or early Polygnathus mehli latus time. Movement on the ENE trending St. Patrick's Well Fault influenced the deposition of the Walterstown Member and the overlying Moathill Formation and was probably associated with the development of the East Midlands depocentre to the south of the area. A second episode of tectonism in the latest Courceyan or early Chadian resulted in uplift and erosion and the development of ‘block and basin’ sedimentation. Subsequent transgression of the uplifted block led to the establishment of the Kentstown Platform, bounded to the north, west and south by rocks of basinal facies. The Milverton Group (Chadian-Asbian), confined to this platform, unconformably overlies Courceyan or Lower Palaeozoic strata and is subdivided into three formations: Crufty Formation (late Chadian), Holmpatrick Formation (late Chadian-Arundian) and Mullaghfin Formation (late Arundian-Asbian). The Walterstown Fault controlled the western margin of the Kentstown Platform at this time. Contemporaneous basinal sediments of the Fingal Group (Lucan and Naul Formations) accumulated to the west of the Walterstown Fault and are much thicker than age-equivalent platform facies. Platform sedimentation ceased in latest Asbian to early Brigantian time with tectonically induced collapse and drowning of the platform; platform carbonates of the Mullaghfin Formation are onlapped northwards by coarse proximal basinal facies of the Loughshinny Formation. A distinct gravity anomaly in the Kentstown area suggests the presence of a granitoid body within the basement. The Kentstown Platform is therefore considered to have formed on a buoyant, granite-cored, footwall high analogous to the Askrigg and Alston Blocks of northern England.  相似文献   

A Carbon Isotopic Stratigraphic Pattern of the Late Palaeozoic Coals in the North China Platform and Its Palaeoclimatic Implications     

ZHANG Hong  SHEN Guanglong  HE Zonglian . Institute of Geology Xi''an Branch  China Coal Research Institute  Northern Yanta Ro  Xi''an  Shaanxi Province  China. . Department of Geology Northwest University  I North Taibai Ro  Xi''an  Shaanxi Province  China Zhu Xiling 《《地质学报》英文版》1999,73(1):111-119

This paper gives the stable carbon isotopic data in coals from the Late Namurian to Kazanian stages inthe Serteng Mt., Xishan and Huainan coalfields of the North China Platform. Its stratigraphic pattern shows that sev-eral isotopic shifts are apparent, and the large δ~(13)C negative shifts (approximately 2.5 to 3.0‰) occurred during theStephanian, Artinskian and Kazanian are observed in three Permo-Carboniferous coalfields. Those negative shifts areneither related to the coal rank and coal macerals, nor caused by the variety of peat-forming plants. The general de-crease in the δ~(13)C values of the Stephanian, Artinskian and Kazanian coals is consistent with an overall decrease inthe δ~(13)C values of ambient atmospheric CO_2 and/or a relative increase in atmospheric P_(CO2) during the coal-forming pe-riods. Therefore the authors postulate that the oxidation of peat, and the δ~(13)C-depleted CO_2 flux into the atmosphereduring the above stages may have contributed to coeval palaeoclimatic warming by way of the greenhouse effect.  相似文献   

Technical Note AIMS (TM): An Alternative Tool for Coastal Mapping     

Dorota A. Grejner-Brzezinska  Charles K. Toth 《Marine Geodesy》1999,22(2):129-137

Space technologies, such as kinematic Global Positioning System (GPS), often combined with an inertial navigation system (INS), provide an efficient direct georeferencing tool for remote sensing and aerial surveying. Practically, these systems are now able to deliver high-precision orientation data for spatial data acquisition platforms in a timely manner, at relatively low cost, as compared to traditional methods. The Airborne Integrated Mapping System (AIMS (TM)), developed at The Ohio State University Center for Mapping, integrates high-resolution digital imagery, differential GPS/INS, and precise timing for high-quality data acquisition supporting large-scale mapping and other precise positioning applications. In this article, the AIMS (TM) system hardware/software configuration, its current operational capabilities, and the test results of airborne mapping of the coastal zone are presented.  相似文献   

Tectonic Evolution of the Northern Continental Margin of North China Platform in Middle Proterozoic     

Xu Zhongyuan  Liu Zhenghong 《世界地质(英文版)》2000,3(1)

An orogenic belt developed in late middle Proterozoic in the northern margin of North China Plate extends from Inner Mongolia to Western Liaoning Province and Eastern Jilin Province. It is over 2000km long. The orogenic belt was formed by collision between North China Platform and Siberia Platform during the Rodinian Super- Continent period. From sedimentary formation, magmatic activity and crustal tectonic deformation, it is suggested that along the tectonic belt the paleocontinental margin experienced four stages of tectonic evolution in middle Proterozoic, they are: continental margin rift,passive continental margin, active continental margin and collisional orogenic stages.  相似文献   

考虑几何非线性的张力腿平台随机响应等效线性化分析     

何勇  金伟良  龚顺风 《海洋工程》2008,26(4)

考虑深海柔性张力腿平台的几何非线性特征,建立柔性平台结构非线性随机振动响应分析方法.该方法结合模态分析,把系统隐式的非线性项转化为由模态坐标高次组合表示的显式非线性项,在此基础上引入虚拟激励法,建立结构在随机波浪荷载作用下的等效线性化系统,从而确定结构各非线性随机响应.通过对某一mini-TLP的分析结果和试验实测值的比较,表明该方法具有较好的计算精度和较快的计算速度,能够满足大型结构的非线性随机响应分析要求.通过对不同波高的计算,结果表明张力腿平台在较大波高作用下几何非线性影响显著,忽略这部分的影响,计算结果将会产生很大的误差.  相似文献   

From Cycles to Sequences:Sequence Stratigraphy and Relative Sea Level Change for the Late Cambrian of the North China Platform     

MEI Mingxiang  MA Yongsheng  DENG Jun  CHEN Huijun Key Laboratory of Lithospheric Tectonics  Lithoprobing Technology of the Education Ministry  China University of Geosciences  Beijing  Department of Oil-Fields  China Petrochemical Corporation  Beijing 《《地质学报》英文版》2005,79(3):372-383

In the Late Cambrian, the North China Platform was a typical carbonate ramp platform. The Upper Cambrian of the northern part of the North China Platform is famous for the development of bioherm limestones and storm calcirudites and can be divided from bottom to top into the Gushan, Changshan and Fengshan formations. In this set of strata, the deep-ramp mudstone and marls and the shallow-ramp packstones and grainstones constitute many carbonate meter-scale cycles of subtidal type. More tidal-flat dolomites axe developed in the Upper Cambrian of the southern margin of the North China platform, in which limestone and dolomite beds also constitute many carbonate meter-scale cycles of the peritidal type. These cycles are marked by a variety of litho-facies successions. There are regularly vertical stacking patterns of meter-scale cycles in long-term third-order sequences, which is the key to discerning such sequences. Third-order sequence is marked by a particular sedimentary-facies succession that is the result of the environment-changing process of deepening and shoaling, which is genetically related to third-order sea level changes. Furthermore, four third-order sequences can be grouped in the Upper Cambrian of the North China Platform. The main features of these four third-order sequences in the northern part of the platform can be summarized as follows: firstly, sequence-boundaries are characterized by drowning unconformities; secondly, the sedimentary-facies succession is generally constituted by one from deep-ramp facies to shallow-ramp facies; thirdly, a succession of “CS (?) HST” (i.e., “condensed section and highstand system”) forms these four third-order sequences. The chief features for the third-order sequences in the southern part of the North China Platform comprises: more dolomites are developed in the HSTs of third-order sequences and also developed more carbonate meter-scale cycles of peritidal types; the sedimentary-facies succession of the third-order sequences is marked by “shallow ramp-tidal flat”; the sequence boundaries are characterized by exposure punctuated surfaces. According to the changes for the third-order sequences from the north to the south, a regular sequence-stratigraphic framework can be established. From cycles to sequences, the study of sequence stratigraphy from litho-facies successions to sedimentary-facies successions exposes that as follows: meter-scale cycles that are used as the basic working unit actually are litho-facies successions formed by the mechanism of a punctuated aggradational cycle, and third-order sequences that are constituted by regularly vertical stacking patterns of meter-scale cycles are marked by sedimentary-facies successions. On the basis of the changing curve of water depth at each section, the curve of the relative third-order sea level changes in the late Cambrian of the North China Platform can be integrated qualitatively from changing curve of water depth. The correlation of Late Cambrian long-term sea level changes between North China and North America demonstrates that there are not only similarities but also differences, reflecting control of long-term sea level changes both by global eustacy and by regional factors.  相似文献