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Zircon and whole-rock Nd-Pb isotopic provenance of Middle and Upper Ordovician siliciclastic rocks, Argentine Precordillera 总被引：1，自引：0，他引：1
JAMES D. GLEASON STANLEY C. FINNEY† SILVIO H. PERALTA‡ GEORGE E. GEHRELS§ KATHLEEN M. MARSAGLIA¶ 《Sedimentology》2007,54(1):107-136
Graptolite‐bearing Middle and Upper Ordovician siliciclastic facies of the Argentine Precordillera fold‐thrust belt record the disintegration of a long‐lived Cambro‐Mid Ordovician carbonate platform into a series of tectonically partitioned basins. A combination of stratigraphic, petrographic, U‐Pb detrital zircon, and Nd‐Pb whole‐rock isotopic data provide evidence for a variety of clastic sediment sources. Four Upper Ordovician quartzo‐lithic sandstones collected in the eastern and central Precordillera yield complex U‐Pb zircon age spectra dominated by 1·05–1·10 Ga zircons, secondary populations of 1·22, 1·30, and 1·46 Ga, rare 2·2 and 1·8 Ga zircons, and a minor population (<2%) of concordant zircons in the 600–700 Ma range. Archaean‐age grains comprise <1% of all zircons analysed from these rocks. In contrast, a feldspathic arenite from the Middle Ordovician Estancia San Isidro Formation of the central Precordillera has two well‐defined peaks at 1·41 and 1·43 Ga, with no grains in the 600–1200 Ma range and none older than 1·70 Ga. The zircon age spectrum in this unit is similar to that of a Middle Cambrian quartz arenite from the La Laja Formation, suggesting that local basement rocks were a regional source of ca 1·4 Ga detrital zircons in the Precordillera Terrane from the Cambrian onwards. The lack of grains younger than 600 Ma in Upper Ordovician units reinforces petrographic data indicating that Ordovician volcanic arc sources did not supply significant material directly to these sedimentary basins. Nd isotopic data (n = 32) for Middle and Upper Ordovician graptolitic shales from six localities define a poorly mixed signal [ɛNd(450 Ma) = −9·6 to −4·5] that becomes more regionally homogenized in Upper Ordovician rocks (−6·2 ± 1·0; TDM = 1·51 ± 0·15 Ga; n = 17), a trend reinforced by the U‐Pb detrital zircon data. It is concluded that proximal, recycled orogenic sources dominated the siliciclastic sediment supply for these basins, consistent with rapid unroofing of the Precordillera Terrane platform succession and basement starting in Mid Ordovician time. Common Pb data for Middle and Upper Ordovician shales from the western and eastern Precordillera (n = 15) provide evidence for a minor (<30%) component that was likely derived from a high‐μ (U/Pb) terrane. 相似文献
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<正>Fourteen graptolite species of the Late Tremadoc and Early Floian are described from the Nanba section in the Yiyang area,Hunan Province.Among them,Paradelograptus onubensis, Kiaerograptus bulmani,K.kutchini and Paratemnograptus isolatus of the Late Tremadoc are first found in China.Based on the current graptolite materials,the correspondingly complete graptolite zones of Upper Tremadocian in China are recognized as follows(in ascending order):the Adelograptus tenellus Zone,the Aorograptus victoriae Zone,the Araneograptus murrayi Zone and the Hunnegraptus copiosus Zone.In the Nanba section,the Hunnegraptus copiosus Zone is overlain directly by the Tetragraptus approximatus Zone,there is no hiatus below the base of Floian. 相似文献
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为响应国际地层委员会奥陶系分会的要求,实现扬子区与江南区奥陶纪晚期—志留纪早期生物地层精时对比,选取位于江南斜坡带的湖南益阳南坝剖面作为研究对象,对志留系底部Parakidograptus acuminatus带笔石进行了系统的研究。剖面内五峰组岩性为黑色页岩,与上覆周家溪群下组整合接触,地层连续无沉积间断。通过连续不间断采集笔石标本,在研究剖面共识别出笔石6属8种,包括:Parakidograptus acuminatus,Normalograptus elegantulus,Nor. mirnyensis,Metabolograptus persculptus,Neodiplograptus parajanus,Neo. guantangyuanensis,Petalithus hamus,Streptograptus cyclodontus。依据获取的笔石标本,初步识别出Metabolograptus persculptus带和Parakidograptus acuminatus带,确定研究剖面时代为晚奥陶世赫南特期—早志留世鲁丹期。 相似文献
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Two graptolite faunas are described from outcrops of the Wagonga Beds near Batemans Bay on the south coast of N.S.W. They are of late Eastonian and early Bolindian age. The faunas have been found in two geographically separate localities and, in spite of structural complexities, it is now suggested that the greater part of the Wagonga Beds was deposited in the Late Ordovician. The chert and volcanicrich Wagonga Beds were accumulated prior to, or as contemporaneous lateral facies equivalents of, the thick undifferentiated Upper Ordovician ‘slates and grey‐wackes unit’ that crops out in the same general region. 相似文献
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前人对笔石的研究主要用于地层划分和沉积环境分析,对笔石与页岩气之间的关系研究甚少。充分利用取心井岩心分析资料、钻井地质资料、实验分析资料和测录井资料,结合不同沉积环境的笔石类型,将JYDA-E井奥陶系五峰组分成4个笔石带(WF1-WF4)、志留系龙马溪组划成6个笔石带(LM1-LM7,LM2缺失),其中WF2-LM4的TOC含量高、有机孔隙发育,属于页岩气有利开发层段。研究发现:笔石的演化和有机质的富集具有相同的沉积环境;笔石的丰度和TOC、有机孔隙度以及气测全烃含量具有正相关关系,笔石的演化对页岩有机质丰度、有机孔的形成具有一定贡献,并在一定程度上影响其含气性,属于页岩气储层评价的一项重要指标。四川盆地五峰组-龙马溪组页岩气形成和笔石的形成演化存在成因上的关联,这对页岩气储层研究具有借鉴意义。 相似文献
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Detailed mapping and biostratigraphic data provide new evidence of a major break below the base of the Caradoc succession along the northern margin of the Harlech Dome in south central Snowdonia. Within this outcrop the sequence is locally complicated by subsequent tectonic and volcanic events, but undisturbed sections indicate a break of at least 10 Ma between upper Arenig and middle, or upper, Llandeilo strata. The break is greatest between two N-S trending fracture systems, the Cwm Pennant Fault Zone in the west and Trawsfynydd Fault Zone in the east, which both have a persistent history of reactivation. Between these two fractures neither Llanvirn nor lower Llandeilo strata occur. This contrasts with the thick, and perhaps complete, sequence preserved in the Cadair Idris district on the southern margin of the dome and suggests that, during Llanvirn times, the Harlech Dome formed a major uplifted and tilted block, with a tectonically active northern margin. Subsequently, uplift and tectonism either ceased before, or was overwhelmed by, the ensuing sea-level rise associated with the gracilis (early Caradoc) transgression. The preservation of ooidal ironstones around the dome suggests that it may have became a large shoal or platformal area at this time. Renewed uplift and erosion along the northern margin of the Harlech Dome during the early Caradoc (gracilis to multidens) led to large-scale disruption of the stratigraphic succession by mass gravity flow and slumping, overprinting and locally accentuating the effects of the earlier hiatus. 相似文献