华北地台东南缘大别山—连云港地区下元古界变质岩岩石化学   总被引：3，自引：0，他引：3  

桑隆康 《地球科学》1991,16(6):651-659

  相似文献   

中国南方早中三叠世岩相古地理   总被引：8，自引：0，他引：8  

冯增昭  鲍志东 《地质科学》1997,32(2):212-220

在各基于剖面的地层学及定量岩石学研究的基础上,采用单因素分析综合作图法,编制出了中国南方早中三叠世飞仙关期(印度期)、嘉陵江期(奥伦期)、雷口坡期(安尼期)和天井山期(拉丁期)的各种单因素基础图件及定量岩相古地理图。在这种古地理图中,各一、二、三级古地理单元的确定都有定量的单因素数据为依据。各期岩相古地理的特征可概括为陆海相间,台盆相间,台中有盆,盆中有台,台中有滩和坪,台盆间有斜坡。各期岩相古地理有明显的继承性和发展性。从早三叠世飞仙关期到中2叠世天井山期,是一个较大的海退过程。这种定量的岩相方地理图,为中国南方中下三叠统的油气勘探提供了科学依据。  相似文献   

The assessment of the hydrocarbon potential and maturity of Silurian intervals from eastern part of Moesian Platform – Romanian sector     

《Marine and Petroleum Geology》2016

The aim of this paper is the assessment of the hydrocarbon potential and maturity of Silurian intervals from the Călăraşi-Bordei Verde-Biruinţa perimeter – East Moesian Platform. All the information gathered from the wells drilled in the mentioned perimeter is used for the evaluation of the “shale gas” potential, too. This major sedimentary basin has all geological conditions for hydrocarbons generation, migration and accumulation. The main conclusions of the all geo-analyses are the following: the XRD analyses show that the samples consist of clay minerals with organic material, the organic matter contained in the samples of the wells shows widely distributed type of organoclasts. In absence of true vitrinite originating from higher plants in these Lower Paleozoic series, the various encountered organic remains consist of Tasmanites, microporous or homogeneous fragments, structured fragments of graptolites, oxidized or naturally rich in oxygen organoclasts inherited from the continent (phytoclasts, fungal remains). The maturity of the Silurian at Ţăndărei borehole is established taking into account the fluorescence of the Tasmanites and the reflectance of graptolites; the maturity increases with depth between 0.70 and 1% eq. VRo. The organic matter of Biruinţa and Călăraşi boreholes is overmature with maturity of around 1.40–1.55% at 400 m in Biruinţa and a maturity increase with depth between 1.85 and 2.05% eq. VRo in Călăraşi borehole. Those values are mainly deduced from vitrinite/graptolite correlation. According to the maturity trend deduced of Călăraşi and Ţăndărei boreholes, the high maturity of Biruinţa for such a low burial (around 400 m) indicates a possible erosion around 3400 m due to uplift. The Silurian studied samples consist of carbonated claystones with an organic matter of type II with relatively low residual TOC content: less than 1.2% weight for the overmature boreholes (Biruinţa and Călăraşi) and less than 1.6% weight in Ţăndărei borehole.  相似文献   

Response Analysis of Tension-Based Tension Leg Platform Under Irregular Waves     

D. S. Bhaskara Rao  R. Panneer Selvam 《海洋工程》2016,(4):603-614

Tension Leg Platform (TLP) is a hybrid structure used as oil drilling and production facility within water depths of 1200 m. The extension of this TLP concept to deeper waters is a challenge and warrants for some innovative design concepts. In this paper, a relatively new concept of TLP which is christened as Tension-Based Tension Leg Platform (TBTLP) and patented by Srinivasan (1998) has been chosen for study. Response analysis of TLP with one tension base under irregular waves for three different sea states has been performed using hydrodynamic tool ANSYS? AQWA?. Results are reported in terms of RAOs, response spectrums for surge, heave and pitch degrees of freedom from which spectral statistics have been obtained. The statistics of TBTLP have been compared with TLPs (without tension base) for two different water depths to highlight the features of the new concept. The effect of viscous damping and loading effects on the RAOs are also investigated.  相似文献   

The Valanginian history of the eastern part of the Getic Carbonate Platform (Southern Carpathians,Romania): Evidence for emergence and drowning of the platform     

《Cretaceous Research》2016

Lower Cretaceous successions that crop out in the eastern part of the Getic Carbonate Platform (Southern Carpathians, Romania) preserve records of the Valanginian events in different settings of the platform. The integrated sedimentological, biostratigraphical, geochemical and mineralogical analysis of the upper Berriasian–Valanginian successions reveal successive stages in the evolution of the carbonate platform: (a) pre-drowning stage of the shallow-shelf and slope settings of the platform; (b) subaerial exposure and karstification; and (c) incipient flooding and drowning of the carbonate platform. Following the subaerial exposure, starting in the middle early Valanginian, the eastern part of the Getic Carbonate Platform experienced a drowning phase documented by iron oxyhydroxides, phosphate and glaucony mineralized discontinuity surface and glaucony-rich sediments disposed on the discontinuity surface. Recognition of the diachronous intra-Valanginian discontinuity surface within the studied successions is based on clear evidences (facies contrast, depositional and diagenetic features, biostratigraphic and taphonomic data, and geometrical relations). The negative–positive carbon isotope excursion is correlated with the global perturbations of the carbon cycle related to the Valanginian “Weissert” episode, and it is documented for the first time in the shallowest parts of the Getic Carbonate Platform. Tectonic activity and eustatic sea-level fluctuations were most probably the main factors that led to fault-block tilting, local emersion and subsequent drowning of the eastern part of the Getic Carbonate Platform during the Early Cretaceous. We infer that the eastern part of the Getic Carbonate Platform was affected by late Berriasian–early Hauterivian extensional tectonics that could be related to the Neo-Cimmerian movements with effects generally recognized in the northern peri-Tethyan areas.  相似文献   

Hydrothermal Mineralization on the Mesoproterozoic Passive Continental Margins of China: A Case Study of the Langshan-Zha''ertaishan Belt,Inner Mongolia, China     

PENG Runmin  ZHAI YushengKey Laboratory of Lithospheric Tectonics  Lithoprobing Technology  China University of Geosciences  Ministry of Education  Beijing 《《地质学报》英文版》2004,78(2)

Most ore-forming characteristics of the Langshan-Zha'ertaishan hydrothermal exhalation belt, which consists of the Dongshengmiao, Huogeqi, Tanyaokou and Jiashengpan large-superlarge Zn-Pb-Cu-Fe sulfide deposits, are most similar to those of Mesoproterozoic SEDEX-type provinces of the world. The characteristics include: (1) All deposits of this type in the belt occur in third-order fault-basins in the Langshan-Zha'ertaishan aulacogen along the northern margin of the North China Platform; (2) these deposits with all their orebodies hosted in the Mesoproterozoic impure dolomite-marble and carbonaceous phyllite (or schists) have an apparent stratabound nature; ores display laminated and banded structures, showing clear depositional features; (3) there is some evidence of syn-sedimentary faulting, which to a certain extent accounts for the temporal and spatial distribution and the size of the orebodies in all deposits and the formation of intrabed conglomerates and breccias; (4) they show lateral and vertical  相似文献   

Hydrothermal Mineralization on the Mesoproterozoic Passive Continental Margins of China: A Case Study of the Langshan-Zha'ertaishan Belt,Inner Mongolia, China     

PENG Runmin  ZHAI YushengKey Laboratory of Lithospheric Tectonics  Lithoprobing Technology  China University of Geosciences  Ministry of Education  Beijing 《《地质学报》英文版》2004,78(2)

Most ore-forming characteristics of the Langshan-Zha'ertaishan hydrothermal exhalation belt, which consists of the Dongshengmiao, Huogeqi, Tanyaokou and Jiashengpan large-superlarge Zn-Pb-Cu-Fe sulfide deposits, are most similar to those of Mesoproterozoic SEDEX-type provinces of the world. The characteristics include: (1) All deposits of this type in the belt occur in third-order fault-basins in the Langshan-Zha'ertaishan aulacogen along the northern margin of the North China Platform; (2) these deposits with all their orebodies hosted in the Mesoproterozoic impure dolomite-marble and carbonaceous phyllite (or schists) have an apparent stratabound nature; ores display laminated and banded structures, showing clear depositional features; (3) there is some evidence of syn-sedimentary faulting, which to a certain extent accounts for the temporal and spatial distribution and the size of the orebodies in all deposits and the formation of intrabed conglomerates and breccias; (4) they show lateral and vertical  相似文献   

Control of Carbonate Sedimentation and Reef Growth in Llandovery Sequences on the Northwestern Margin of the Yangtze Platform, South China     

Li Yue  Steve Kershaw  Chen Xu   《Gondwana Research》2004,7(4):937-949

The later Telychian (late Llandovery, Silurian) sea-level highstand was a suitable setting for global carbonate deposition and reef growth in epeiric seas. However, evidence from the northwest margin of Yangtze Platform indicates that small carbonate platforms developed in rapidly-subsiding small basins and were principally controlled by muddy clastic input. In particular, sediments of the Ningqiang Formation, late Telychian, usually more than 2000 m thick, are mostly shales, but eight major units of discontinuous (15 km maximum width) and relatively thin (120 m maximum thickness) reef-bearing carbonates, which developed when the sedimentation rate apparently lessened, occur within a relatively short time interval. This interval is between upper griestonensis to spiralis-grandis graptolite biozones, estimated as a c. 2 Ma duration. More than 30 small- to medium-scale patch reefs occur in several parts of the sequence, but only within the carbonate units. Shelly faunas common throughout the sequence reveal water depth to have been shallow during deposition of the Ningqiang Formation equivalent to BA2–3, which has a depth range from low intertidal to the base of the photic zone. BA3 is interpreted as being no more than 60 m deep (Boucot, 1975), which is above normal wave base, frequently affected by storms (Chen et al., 1996), and is regarded as optimum depth for high diversity of Silurian faunas (Boucot, 1975; Brett, 1991). Thus, the rate of sediment accumulation kept pace with basement subsidence, and was a substantial factor for limiting reef growth. Sharp contacts between carbonate units and shales indicate that carbonate units are constrained by frequent inputs of terrigenous debris, as the major cause for termination of carbonate deposition. Therefore, carbonate platforms, and reefs they contained, formed during times when sediment input to the basin lessened and ended when it increased; present evidence does not allow correlation to modeled dry episodes, and we interpret the control to be principally tectonic. Overall, sedimentation in the region was terminated by the end of Telychian time by tectonic uplift of the Yangtze Platform; the southwestward migration of palaeocoastline shows this progression. Sedimentation ceased until Middle Devonian time. Ludlow marine transgression has been recognized in the offshore area of Ningjiang Bay.  相似文献   

蓝细菌繁荣滋养的苗岭世光养碳酸盐岩工厂:以安徽寿县卧龙山剖面崮山组为例     

梅冥相 《地质学报》2021,95(12):3571-3591

描述、界定和解释无穷多样的碳酸盐岩始终是一个谜团,因为许多复杂的问题只有推测性的答案.碳酸盐生产作用体系形象化地定义为碳酸盐岩工厂,最原始的定义是指小于15 m深的清澈浅水环境,因为这是绝大多数碳酸盐生产者的聚居地;后来,基于能量来源,对海相碳酸盐岩工厂提出了一个富有智慧的双重划分,即光养工厂和异养工厂.随着对碳酸盐沉淀作用样式的深入了解,产生了浅海碳酸盐岩工厂或生产作用体系的三重划分,而且被进一步形象化地简称为:①T-工厂,T源于热带或水柱顶部的涵义;②C-工厂,C代表着冷水或受到控制的沉淀作用;③M-工厂,在这里M意味着微生物、泥晶和泥丘.寒武纪苗岭世浅水碳酸盐岩工厂,具有以下两个方面的特殊性:首先是光养的,其次是微生物的(蓝细菌繁荣所滋养的),因此可以识别出两个特别的工厂,即光合作用生物膜诱发的放射鲕粒主导的光养T工厂、以及占据着T-工厂位置的蓝细菌微生物席建造的微生物礁主导的光养-M工厂.安徽寿县卧龙山剖面的寒武系苗岭统崮山组,从凝缩段的陆棚相泥岩变浅至强迫型海退体系域浅缓坡相鲕粒滩相灰岩和均一石主导的微生物礁灰岩,形成一个淹没不整合面所限定的三级层序.一个从微生物放射鲕粒滩到均一石主导的微生物礁的沉积序列,组成了该层序的强迫型海退体系域.下部的放射鲕粒主导的鲕粒滩相灰岩,在鲕粒核心、鲕粒皮层以及鲕粒间的泥晶团块或凝块之中,表现出高密度保存的而且较为肯定地类比于现代织线菌的丝状葛万菌化石,表明了光合作用生物膜诱发了放射鲕粒皮层的放射纤维状方解石的沉淀作用,所以不能理解为非生物成因的沉淀物,从而进一步表明鲕粒滩相灰岩代表着一个特别的光养-T工厂;覆盖在鲕粒滩相灰岩之上的均一石主导的微生物礁,也发育着高密度保存而且占据着超过一半体积或面积的丝状葛万菌,从而代表着一个占据着T-工厂位置的特别的光养M-工厂.因此,一个特别的从光养T-工厂到光养M-工厂的演变序列,发育在寒武纪苗岭世较高的大气圈二氧化碳和氧气含量之下的蓝细菌繁荣的方解石海之中.这些现象和重要发现,为进一步了解寒武纪时期与生物矿化作用得到进化的寒武纪后生动物大爆发相重合、以及与蓝细菌繁荣相关联的有机矿化作用产生的光养微生物碳酸盐岩工厂,提供了一个较为罕见的实例.  相似文献   

Microencruster-microbial-cement framework of the Upper Jurassic reef developed on the slope of the intra-Tethyan carbonate platform (Bulgaria)     

Bogusław Kołodziej  Daria Ivanova 《Proceedings of the Geologists' Association. Geologists' Association》2021,132(2):158-169

The carbonate succession in the Lyalintsi section of the western Moesian Platform (western Bulgaria) displays a shallowing-upward trend. Growth of the Tithonian–Valanginian coral biostromes and low-relief bioherms was preceded by Oxfordian–Kimmeridgian sedimentation of fine-grained peloidal-bioclastic limestones and Saccocoma-bearing limestones on the homoclinal ramp and the carbonate platform slope. In the late Kimmeridgian, boundstones with very rare corals, but with easily recognisable biohermal morphology, were developed. The main components of this reef are encrusting microorganisms, microbial crusts and synsedimentary cements. Microencrusters Labes atramentosa, Crescentiella morronensis, Perturbatacrusta leini and Radiomura cautica, as well as thin crusts of calcified sponges (sclerosponges), are the main biotic components. Corals (almost exclusively microsolenids) are sparse, whereas photophilic microencrusters (e.g., “Lithocodium–Bacinella”), are absent, although they are common in the overlying shallow-water part of the Lyalintsi sequence. Microbialites and synsedimentary cements provided additional support for the reef framework. The framework, especially the biotic components, and the reefal facies position within the sedimentary succession, implies that the high-energy upper slope of the carbonate platform was the depositional setting of the microencruster-microbial-cement reef studied. Encrusting microorganisms, except for C. morronensis and sponges, are only known from the intra-Tethyan platforms. This study supports conclusion of studies of coeval Alpine reefs that the presence of the microencruster-microbial-cement framework provides insight into the palaeobathymetry, palaeogeography and tectonic configuration of the intra-Tethyan carbonate platforms.  相似文献