Correlation of late Cretaceous calcareous nannofossil zones with ammonite zones and planktonic Foraminifera: the Austrian Gosau sections     

M. Wagreich 《Cretaceous Research》1992,13(5-6)

The late Turonian to early Campanian calcareous nannofossil biostratigraphy of the Austrian Gosau Group is correlated with ammonite and planktonic foraminiferal zones. The standard Tethyan zonations for nannofossils and planktonic foraminifers are applied with only minor modifications. The basal marine sediments of the Gosau Group, bearing late Turonian-early Coniacian macrofossils, belong to the Marthasterites furcatus nannofossil Zone (CC13). The Micula decussata Zone (middle Coniacian to early Santonian) is combined with the Reinhardtites anthophorus Zone because of the rare occurrence of Renhardtites cf. R. anthophorus already in the Coniacian and taxonomic problems concerning the correct identification of this species. The Santonian-Campanian boundary lies within the Calculites obscures Zone (CCl7).  相似文献   

华北地台北缘中段中上志留统与白乃庙群接触关系及其滑断构造     

曾庆栋 《吉林地质》1992,11(4):36-42

华北地台北缘中段中上志留统与中元古代自乃庙群接触关系为角度不整合,且沿角度不整合面发生了构造叠加作用,产生了滑断构造。该滑断构造具有宏观、微观变形组构,并且控制了一系列金矿点(矿化点)的分布,是一条重要的金矿化带。  相似文献   

芦山—天全地区大溪砾岩岩石学特征及物源区分析     

李元林  纪相田 《矿物岩石》1993,13(3):68-73

大溪砾岩为一套厚层碳酸盐质砾岩,具有砾石含量高,砾石分选、磨圆较好的特点。据砾石统计、薄片分析、古生物鉴定、古流分析及重矿物组合表明,大溪砾岩中砾石主要来自龙门山区的泥盆系—三叠系,填隙物中的石英碎屑可能主要来自杂岩体。大溪砾岩的砾石成分有向上趋于复杂的特点。  相似文献   

Calcareous　Algae　from　Northeastern　Brilon　Reef　Complex　of　Middle　and　Upper　Devonian　in　Eastern　Sauerland，　Germany     

Hong Tianqiu 《中国地质大学学报(英文版)》1994,(1)

ＣａｌｃａｒｅｏｕｓＡｌｇａｅｆｒｏｍＮｏｒｔｈｅａｓｔｅｒｎＢｒｉｌｏｎＲｅｅｆＣｏｍｐｌｅｘｏｆＭｉｄｄｌｅａｎｄＵｐｐｅｒＤｅｖｏｎｉａｎｉｎＥａｓｔｅｒｎＳａｕｅｒｌａｎｄ，Ｇｅｒｍａｎｙ￥ＨｏｎｇＴｉａｎｑｉｕ（ＤｅｐａｒｔｍｅｎｔｏｆＲｅ...  相似文献   

Calcareous phytoplankton from the Barremian/Aptian boundary interval in NW Germany     

Helmut Keupp  Jrg Mutterlose 《Cretaceous Research》1994,15(6)

Two cored boreholes in the central part of the North West German Basin recovered a unique section of Upper Barremian to Lower Aptian strata. Calcareous nannofossils show a distinctive shift from boreal endemic assemblages in the Barremian to cosmopolitan ones in the Aptian. This onset of new cosmopolitan species (e.g., Chiastozygus litterarius, Flabellites oblongus, Rhagodiscus angustus, Braarudosphaera sp., Eprolithus sp.) is spread over an interval of 25m, starting well below the early Aptian "Fischschiefer", a dark laminated shale rich in organic matter. These changes in the composition of calcareous nannofossils indicate that major palaeoceanographic changes occurred before the deposition of the Fischschiefer.The distribution pattern of calcispheres allows the differentiation of two sedimentary successions, separated by the Fischschiefer. The lower succession, which includes the sediments below the base of the Fischschiefer, indicates a boreal-pelagic environment. The lower part of the upper successions which includes the Fischschiefer, represents warmer inner shelf conditions. This corresponds to the presence of rich Tethyan-derived nannoconid assemblages and the presence of the planktonic foraminifera Hedbergella in the Fischschiefer. The topmost part of the upper succession (middle Aptian, Hedbergella marl) suggests a change to a pelagic warmer water environment. Two new taxa are introduced: the calcareous dinoflagellate cyst Obliquipithonella laqueata n. sp. and the foraminiferan Choanaella fortunate n. gen. n. sp.  相似文献   

尧峪金铜矿超厚水敏性地层钻进泥浆护壁技术          下载免费PDF全文

陈伟武 《探矿工程》2013,40(5):38-40,43

尧峪金矿区超厚水敏性风化层,在钻进过程中遇到坍塌、掉块、事故频繁发生等问题,采用常规护壁措施并没有取得预想的效果。通过试验应用PAB不分散聚合物泥浆和钾基处理的聚合物泥浆,取得了良好的效果,顺利完成了ZK604孔的钻探施工,为该矿区今后的钻探工作提供了一些可供参考的经验。介绍了该矿区钻探施工的难题以及采取的泥浆技术措施。  相似文献   

南化塘区晚震旦世碳酸盐砾岩层序及其形成机制探讨     

李侠  胡健民  宋子新  刘护军 《地球科学与环境学报》1993,(Z1)

作者认为鄂西南化塘区晚震旦世发育的一套碳酸盐砾岩层序,是碳酸盐台地上台隆边缘形成的一种特殊沉积岩相,是古海洋面强烈波动的一种标志。文章从构造学和沉积学方面初步探讨了其建造过程和形成机制。  相似文献   

Occurrence of gold in hydrothermal pyrite,western Taupo Volcanic Zone,New Zealand     

Youjun Zhang  Lu Wang  Jianwei Li  Peng Feng  Yang Huang 《Geodinamica Acta》2016,28(3):185-198

The Taupo Volcanic Zone (TVZ) on the North Island of New Zealand is located above the subducting Pacific slab and hosts hydrothermal systems related to subduction, arc magmatism and crustal extension. In these systems, gold is transported primarily as sulphide complexes, with gold being deposited in response to boiling and mixing of the deep geothermal fluids. Conglomerate cobbles and hydrothermal fumaroles from the upper Retaruke River in the western TVZ are mineralised deposits that have been eroded from the nearby Miocene alluvial sedimentary plateau. Abundant gold-bearing pyrite was precipitated in the conglomerates and fumaroles by late hydrothermal process, primarily occurring as veinlets, disseminations and fine-grained aggregates which consists discrete euhedral microcrystals. Scanning electron microscopy combined with X-ray energy disperses spectroscopy shows that pyrites are commendably affected by late hydrothermal fluids, possibly by the carbonate fluid. Electron probe microanalysis revealed that the pyrite contains 20–120 ppm Au (averaging 60 ppm). Wavelength dispersive spectral elemental mapping suggests that gold is distributed uniformly in pyrite, indicating structurally bound gold (solid solution) in pyrite. Gold mineralisation recognised in the conglomerates and fumaroles demonstrates that the upper Retaruke River is a promising target for future gold exploration.  相似文献   

西沙群岛西科1井第四纪钙藻及其生态功能   总被引：2，自引：0，他引：2       下载免费PDF全文

马兆亮  祝幼华  刘新宇  罗威  马瑞芳  徐守立 《地球科学》2015,40(4):718-724

对西沙群岛西科1井第四纪地层中的钙藻进行了初步研究, 共鉴定钙藻3科7属, 包括红藻门珊瑚藻科让氏藻属、蟹手藻属、珊瑚藻属、石枝藻属和石孔藻属, 以及绿藻门松藻科仙掌藻属和粗枝藻科伞轴藻属.通过对地层中钙藻形态功能的分析, 西科1井第四纪早期海水较深, 沉积环境为礁前相, 中期外礁坪和内礁坪交替沉积, 至晚期出现短时间的泻湖相之后沉积环境演变为礁后滩相.西科1井第四纪钙藻在造礁功能上主要体现在2个方面: (1)通过自身的钙化作用, 为生物礁的生长供应微小碳酸盐颗粒沉积物; (2)利用自身形成的节片结构和生物捆扎-粘结结构参与造礁.   相似文献   

海水环境下巴氏芽孢杆菌驯化及钙质砂固化效果研究     

肖瑶  邓华锋  李建林  程雷  朱文羲 《岩土力学》2022,(2):395-404

为了提升微生物诱导碳酸盐沉淀(MICP)技术在海洋环境下对钙质砂的加固效果,在以往研究的基础上,设计进行了人工海水环境下巴氏芽孢杆菌多梯度人工驯化培养试验,并结合MICP固化钙质砂柱的力学试验和微细观结构分析,对巴氏芽孢杆菌的驯化效果进行了综合评价。结果表明:(1)海水环境下五梯度驯化后细菌的菌液浓度可达到淡水环境的97%以上,其与胶结液作用后碳酸盐的生成量较淡水环境下有一定幅度提高;(2)驯化后的巴氏芽孢杆菌具有很好的温度适应能力,在10～30℃温度下均有较好的MICP性能;(3)海水环境下加固的钙质砂柱无论是碳酸盐生成量还是无侧限抗压强度均较未驯化前高,尤其是五梯度驯化后的细菌,驯化后的细菌菌体变小,在海水环境生成的碳酸盐(碳酸钙和碳酸镁)晶体更小,更加致密,能更好地填充钙质砂颗粒的孔隙并胶结相邻的钙质砂颗粒,具有更优异的MICP性能。相关研究思路和方法可为MICP技术在海洋环境钙质砂地基加固方面的研究与应用提供参考。  相似文献