中国南部奥陶—志留纪笔石页岩相类型及其构造古地理   总被引：3，自引：1，他引：3  

李志明  全秋琦 《地球科学》1992,17(3):261-269

  相似文献   

Correlations among the reflectances of vitrinite, chitinozoans, graptolites and scolecodonts     

Rudolf Bertrand 《Organic Geochemistry》1990,15(6)

Paleozoic marine sequences sampled in outcrops and wells of northeastern Gaspe Peninsula (Quebec Appalachians) yield kerogen composed in part of vitrinite and zooclasts (chitinozoans, scolecodonts and graptolites) on which reflectance measurements were made.The comparison between means of random measurements show that reflectance of chitinozoans is similar to that of telinite (vitrinite with a cellular texture) and that the reflectance of scolecodonts is significantly lower than that of telinite in the lower range of studied values. At higher reflectivities differences decrease but, at the end of the condensate gas zone reflectancea are not yet identical. As shown by previous studies, reflectance of graptolites is slightly less than that of telinite.Pyrobitumen reflectance is related to the lithology of the host-rock and no generalized correlation can be established between the reflectance of pyrobitumen and that of vitrinite.  相似文献   

中国南方五峰组-龙马溪组页岩中笔石与有机质富集关系探讨   总被引：1，自引：0，他引：1  

邱振  董大忠  卢斌  周杰  施振生  王红岩  吝文  张晨晨  刘德勋 《沉积学报》2016,34(6):1011-1020

中国南方奥陶纪-志留纪之交广泛沉积了以五峰组和龙马溪组为代表的笔石页岩。基于对重庆巫溪地区五峰组-龙马溪组底部页岩段中近400件页岩样品中笔石丰度的统计及100件页岩样品有机碳含量（TOC,%）的分析测试结果,选择其中23件不同笔石丰度与TOC的页岩样品开展页岩中笔石体与围岩（非笔石体部分）TOC的对比实验,并结合能谱分析测试结果,探讨笔石与有机质富集的关系。初步研究认为:①五峰组-龙马溪组页岩中笔石体的C、O等元素含量较高,其TOC明显高于围岩,是页岩有机质的贡献者之一;②五峰组-龙马溪组页岩全岩TOC与笔石丰度及笔石体TOC相关性均较差,而与围岩TOC相关性较好,这指示着页岩中笔石丰度对有机质富集影响较小。  相似文献   

西昆仑坎地里克地区奥陶纪含笔石地层的发现     

王朴 《地层学杂志》2001,25(2):123-124

首次报道西昆仑坎地里克地区奥陶纪的含笔石地层 ,并建立秋久博依那克组 ,其时代属晚奥陶世卡拉道克(Caradoc)期  相似文献   

全球下奥陶统-中奥陶统界线层型候选剖面——宜昌黄花场剖面研究新进展   总被引：1，自引：0，他引：1  

汪啸风 Stouge S．陈孝红  李志宏王传尚 ErdtmannB．-D．曾庆銮  周志强陈辉明张淼  徐光洪 《地层学杂志》2005,29(B11):i0003-i0008

湖北宜昌黄花场剖面是我国奥陶系大湾阶的界线层型剖面，高精度生物地层以及岩石、层序地层和碳同位素地球化学的综合研究表明，该剖面完全符合关于建立全球下奥陶统一中奥陶统界线（即奥陶系第三个尚待正式命名的阶）界线层型剖面和点位（GSSP）的条件。建议以该剖面牙形石Baltoniodus？triangularis的首现层位，作为划分全球下奥陶统一中奥陶统界线的GSSP。所建议的GSSP交通方便，位于距宜昌市北北东22km的公路旁，地层出露完美无缺，界线生物层位于大湾组下段SHod-16层底部，距大湾组底部10．57m；界线上下发育了B．？triangularis的完整演化序列，并伴生有极好的Baltoniodus、Trapezognathus、Periodon和Microzarkodina等牙形石属种演化序列来作为佐证；界线之上0．2m所出现的世界广布的Microzarkodina abellum可作为划分此界线的辅助标志。界线生物层位于低位海侵序列之中，界线之下0．6m处所显示的从高位到低位的层序转换面和碳同位素最大偏移，与全球此时所发生低位事件密切相关，可作为识别该界线的物理和化学标志。所建议的界线生物层与笔石Azygograptus suecicus生物带上下组合之间的界线接近，与几丁虫Belonechitina cf．henryi生物带底界几乎一致，因此，所建议的界线易于在全球，无论浅水碳酸盐相、还是深水笔石相，识别和进行精确对比。同样的生物组合序列和层序及碳同位素异常亦在黄花场剖面之北5km的陈家河（即大坪）剖面得到了验证．  相似文献   

论北天山西段奥陶纪含笔石地层及笔石群的划分     

乔新东 《新疆地质》1989,(1)

笔者把下奥陶统新二台组分为三个岩性段,下奥陶统新建五个笔石带、北天山西段以笔石带化石的混生为显著特点,除巳公布的Cardiograptus-Oncograptus混生外,Anisograptus和Triograptus的混生为一新的例证、Anisograptus和Triograptus在我国华南它们分别是新厂期X_1和X_2的笔石带化石,而在果子沟它们上延到相当华南新厂期X_3的层位、此两笔石属的个别分子可继续上延到Tetragraptus(Etagraptus)approximatus带的底部和T.fruticosus带、风沟组被厘定为中奥陶统下部.在科古琴地区发现有中奥陶统上部层位和晚奥陶世地层.  相似文献   

恭城地区奥陶纪地层的初步划分对比     

王建辉  唐兰  唐荣富 《南方国土资源》2001,14(1):32-35

文章以大量新发现的笔石动物群 (共 2 1属、2 4种 )对恭城地区奥陶纪地层进行划分、对比 ,建立起 5个笔石化石带 ,其中Peterograptuselegans为广西境内首次新发现的化石带。  相似文献   

Facies development,depositional settings and sequence stratigraphy across the Ordovician–Silurian boundary: a new perspective from the Barrandian area of the Czech Republic     

Petr &#x;torch 《Geological Journal》2006,41(2):163-192

The Hirnantian and Llandovery sedimentary succession of the Barrandian area has been assigned to middle and outer clastic‐shelf depositional settings, respectively. Deposition was influenced by the remote Gondwanan glaciation and subsequent, long‐persisting, post‐glacial anoxia triggered by a current‐driven upwelling system. High‐resolution graptolite stratigraphy, based upon 19 formally defined biozones—largely interval zones—and five subzones, enabled a detailed correlation between 42 surface sections and boreholes, and enabled linking of the sedimentary record, graptoloid fauna dynamics, organic‐content fluctuations and spectral gamma‐ray curves. The Hirnantian and Llandovery succession has been subdivided into four biostratigraphically dated third‐order sequences (units 1–4). Time–spatial facies distribution recorded early and late Hirnantian glacio‐eustatic sea‐level lowstands separated by a remarkable mid‐Hirnantian rise in sea‐level. A major part of the post‐glacial sea‐level rise took place within the late Hirnantian. The highstand of Unit 2 is apparently at the base of the Silurian succession. Short‐term relative sea‐level drawdown and a third‐order sequence boundary followed in the early Rhuddanian upper acuminatus Zone. Early Aeronian and late Telychian sea‐level highstands and late Aeronian drawdown of likely eustatic origin belong to units 3 and 4. Sea‐level rise culminated in the late Telychian, which may also be considered as a highstand episode of a second‐order Hirnantian–early Silurian cycle. Facies and sequence‐stratigraphic analysis supports recent interpretations on nappe structures in the core part of the Ordovician–Middle Devonian Prague Synform of the Barrandian. Copyright © 2006 John Wiley & Sons, Ltd.  相似文献   

早-中奥陶世之交笔石动物群全球分布及其控制作用     

王传尚  汪啸风 《地质科技情报》2011,30(2):41-44,51

为研究笔石动物群在早一中奥陶世之交全球分布的控制因素,从以下3个方面进行了分析和研究:①分析了穿越扬子地台笔石动物群的分布特征;②在对笔石体形态功能分析的基础上,探讨了水体深度对笔石动物群分布的影响;③根据当时的古地理格局,并参考现今的洋流分布,建立了早一中奥陶世之交的洋流分布图.在以上研究的基础上,对前人以水体深度作...  相似文献   

关于强壮弓笔石(Cyrtograptus robustus)的补充研究     

王健  孟勇  王欣  黄洪平  傅力浦  张欣 《地质通报》2011,30(8):1233-1237

在陕西紫阳新发现一块更为完整的强壮弓笔石(Cyrtograptus robustus)化石,对其始部、主枝、幼枝、胞管等特征进行了描述和数据统计,并与国内外相似的弓笔石进行对比。该种弓笔石主枝较宽,一级幼枝发育,相邻幼枝间隔胞管数为1~7个不等,随着主枝的延伸相邻幼枝间隔胞管数增大。笔石体没有二级幼枝,胞管形态为较矮的三角形。该种化石的补充研究为C. lapworthi带的弓笔石种类和弓笔石早期发育情况的研究提供了重要的基础资料。  相似文献