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991.
本文报道在东昆仑地区发现的一种较为稀少的含石榴石英云闪长玢岩,这也是此类岩石在中国的首次发现。该次火山岩形成于晚三叠纪,主要由富钙(CaO5 wt%)、贫锰(MnO3 wt%)的石榴石,富铝的角闪石(15.9 wt%),中性斜长石和石英等斑晶以及基质物质组成。岩石含有中等的SiO_2(61.1~62.2wt%),低的MgO(2.0 wt%),K_2O(1.3 wt%)以及较高的Al_2O_3(17 wt%)含量,呈现出次铝质至轻微过铝质的特征(ACNK=0.89~1.05)。在微量元素方面,该岩石富集大离子亲石元素和轻稀土元素,同时亏损Nb-Ta-Ti,显示出典型的消减带特征。而异常低的重稀土(Yb0.8×10~(-6))和相对高的Sr/Y比值(约38)表明石榴石是一个残留相,而较高的Al_2O_3含量,大多为正的铕异常反映了斜长石因结晶受到抑制而在岩浆演化晚期的聚集,同时表明岩浆具有较高的水含量。Nd-Sr同位素组成(ε_(Nd)(t)=-2.33~-1.38;~(87)Sr/~(86)Sr=0.706 5~0.706 7)和斜长石的反向分带显示,壳幔间岩浆混合作用在岩体的形成过程中扮演了重要角色。石榴石斑晶和其中的钛铁矿包体均含有较低的MgO,且包裹石榴石的角闪石形成于较高的压力(8~10 kb)条件下,显示这些矿物结晶自一个长英质岩浆中,且很可能形成于壳幔过渡带附近。尽管该岩石在富铝、低重稀土、高Sr/Y等很多方面均类似于埃达克岩石,但其中等含量的Sr(260×10~(-6))和La/Yb比值(16~21)却明显低于典型的埃达克岩和太古代的TTG。结合石榴石斑晶中广泛存在的磷灰石包体以及其较高的Sr和轻稀土分配系数,本文提出在岩浆演化早期结晶的磷灰石有效地降低了残余熔体中的Sr和轻稀土。这进一步表明,即使在高水逸度的条件下,磷灰石在岩浆早期的大量结晶可以有效地阻止一些弧岩浆演化成为埃达克质岩石。 相似文献
992.
黑色页岩样品中痕量级铂族元素地球化学成分标准物质研制 总被引:2,自引:2,他引:0
介绍了黑色页岩样品中6个铂族元素铂、钯、钌、锇、铑、铱的标准物质研制过程。黑色页岩样品采自贵州黄家湾,为一次采集、一次混样的原始样品,随机抽取包装好后的样品进行检验与定值。均匀性、稳定性符合要求后,按照国际标准化组织(ISO)34、35指南的基本要求和我国一级标准物质的技术规范,采用多个实验室协同测试的定值方式,利用不同原理的分析方法对此样品的6个铂族元素进行定值。以各实验室组数据作为最小统计单元,用Grubbs准则、Dixon法检验剔除离群数据,Shapiro-Wilk法检验各元素数据分布的正态性。检验结果100%的元素呈正态或近似正态分布。定值的6个元素均符合标准值水平。 相似文献
993.
994.
A novel method is presented for the wavelength calibration of the Large Sky Area Multi-Object Fiber Spectroscopic Telescope (LAMOST). The proposed method combines the arc lines and night sky lines, and can achieve high performance. Firstly, the initial wavelength calibration is performed by employing arc lines. Afterwards, the centroids of sky lines are calculated by the initial calibration results and adjusted by the gravity method iteratively. Finally, the ultimate wavelength calibration is obtained by fitting the centroids of arc lines and sky lines with their corresponding wavelengths. Experiments are performed on the data observed by LAMOST, and the results of the proposed method are more accurate than that of the calibration only by arc lines or sky lines. The calibration sky lines are dense in the red channel (5,700–9,000 Å) of LAMOST, but only a few ones are in the blue channel (3,700–5,900 Å). The new method achieves excellent results in the red channel as the substantial sky lines are employed, and the calibration accuracy of the blue channel is also enhanced in some degree by the scare sky lines. 相似文献
995.
辽上金矿床位于胶东新发现的胶莱盆地东北缘成矿区之内,为胶东东部首例特大型金矿。矿区金成矿以充填作用为特征,载金矿物主要为自形—半自形结构黄铁矿和白云石,以网脉状、细脉状、微细脉状黄铁矿白云石细脉形式出现于岩石碎裂隙中,或以黄铁矿白云石大脉状充填于断裂构造中。矿石包括含金黄铁矿白云石脉型和含黄铁矿白云石脉蚀变岩型2大类。通过对比认为,该矿床为一新类型,即黄铁矿白云石脉型金矿床。这一新类型特大型金矿的发现,预示着胶莱盆地边缘地区具有较好的找矿前景,尤其在金牛山地区应有可能在短期内取得更大的找矿突破。 相似文献
996.
The Yitong Basin is an oil-bearing basin with unique characteristics in Northeast China. On the basis of apatite fission track ages and geological relationship, the tectonic uplift history of the Yitong Basin since the Oligo-cene was discussed. Based on apatite fission track analysis of five samples from the Luxiang and Chaluhe fault de-pressions and basin modeling study, it can be concluded that since the Oligocene (36.6 Ma) in the Yitong Basin, the Chaluhe fault depression has undergone two episodes of uplift during 24.9–19.1 Ma and 6.9–4.9 Ma. And the Luxi-ang fault depression also had undergone two episodes of uplift during 30–27.8 Ma and 22.6–11.1 Ma. Moreover, the average apparent exhumation rates for the Chaluhe fault depression and Luxiang fault depression, could be calcu-lated to be 70.34 and 60.33 m/Ma since 21.8 Ma and 18.9 Ma, respectively. The results of thermochronological analysis can also be supported by the evidence from geological relationships such as geodynamics, volcanic activity, and stratigraphic division and correlation. 相似文献
997.
998.
东胜砂岩型铀矿床是近几年在中国鄂尔多斯盆地东北部发现的一大型铀矿床。因其独特的特征而不同于其他普通砂岩型矿床,矿体一般受绿色砂岩和灰色砂岩之间的过渡带控制,而这两种砂岩目前都指示着还原地球化学环境。古氧化绿色砂岩主要由与油-气二次还原作用有关的绿泥石化和绿帘石化造成。从成因上讲,该矿床与普通砂岩型铀矿床不同,它有着更为复杂的成因,不仅经历了古氧化的成矿过程,而且还经历了油-气流体和热液流体的再改造。空间上,它与侏罗纪直罗组辫状古河道体系有关。较高品位的铀矿化带一般赋存在辫状河主河道与分支河道的分叉部位,所形成砂岩的不均匀性表明,其沉积相属于辫状河到辫状三角洲的过渡沉积体系。统计结果表明,中、细粒砂岩是铀矿化最有利的岩石类型。 相似文献
999.
G. A. Shatkov N. G. Berezhnaya Ye. N. Lepekhina N. V. Rodionov I. P. Paderin S. A. Sergeyev 《Doklady Earth Sciences》2010,432(1):587-592
The precision dating (U-Pb local by zircons, SHRIMP-II) of volcanic rocks in the unique uranium-bearing structure of Transbaikalia
is performed for the first time. The basic conclusions are as follows. The volcanic activity in the Tulukuev caldera covers
the period of not less than 30–35 mln years, within the period from (not later than) 162 to 128 mln years. Two stages of caldera
evolution are established: the early (trachydacite-basalt) stage up to 154 mln years and the late (trachybasalt-rhyolite)
stage from 142 to 128 mln years, with a 10 mln year break, which caused the deep erosion of the lower layer. Three phases
of rhyolite magmatism are substantiated. The first one, 142 mln years, is the ejection of ignimbrites (microfelsitic rhyolites);
the second one, 137–135 mln years, is the outflow of lavas of sanidine-morion rhyolites and subvolcanic and ring dyke intrusions.
The third phase, 128 mln years, is connected with the occurrence of cesium-bearing perlites in the southwestern part of the
caldera. The age of the granite-porphyries of the Krasnokamensk stock almost coincides with the precision data of the age
of the uranium ores [4]. It is found that zircons from the granite-porphyries within the ore field of the Argunsk deposit
have an anomalously high content of uranium. This fact can additionally testify to the time-and-spatial closeness of magmatism
and processes of ore formation. 相似文献
1000.
Yeşim İslamoğlu Mathias Harzhauser Martin Gross Gonzalo Jiménez-Moreno Stjepan Coric Andreas Kroh Fred Rögl Jan van der Made 《International Journal of Earth Sciences》2010,99(1):183-200
The Oligocene depositional history of the Thrace Basin documents a unique paleogeographic position at a junction between the
Western Tethys and the Eastern Paratethys. As part of the Tethys, shallow marine carbonate platforms prevailed during the
Eocene. Subsequently, a three-staged process of isolation started with the Oligocene. During the Early Rupelian, the Thrace
Basin was still part of the Western Tethys, indicated by typical Western Tethyan marine assemblages. The isolation from the
Tethys during the Early Oligocene is reflected by oolite formation and endemic Eastern Paratethyan faunas of the Solenovian
stage. The third phase reflects an increasing continentalisation of the Thrace Basin with widespread coastal swamps during
the Late Solenovian. The mollusc assemblages are predominated by mangrove dwelling taxa and the mangrove plant Avicennia is recorded in the pollen spectra. The final continentalisation is indicated by the replacement of the coastal swamps by
pure freshwater swamps and fluvial plains during the Late Oligocene (mammal zone MP 26). This paleogeographic affiliation
of the Thrace Basin with the Eastern Paratethys after ~32 Ma contrasts all currently used reconstructions which treat the
basin as embayment of the Eastern Mediterranean basin. 相似文献