呼伦湖早白垩世碱性流纹岩的地球化学特征及其意义   总被引：34，自引：2，他引：34       下载免费PDF全文

葛文春  李献华  林强  孙德有  吴福元  尹成孝 《地质科学》2001,36(2):176-183

大兴安岭呼伦湖一带的上库力组第3段流纹岩具有高硅(SiO₂=75.41%～77.32%)、富碱(Na₂O+K₂O=7.98%～8.74%)、富Y、Nb、Zr及低Al、Mg、Ca、Ni、Cr、Ti和高Ga/Al比值等特点,类似于A型花岗岩,而与高度分异的I型和S型花岗岩有明显差别。该流纹岩的地球化学特征类似于A₁型花岗岩,且与该区A型花岗岩同时,很可能是A型花岗岩浆喷出相的产物。流纹岩的全岩Rb-Sr等时线年龄127±5Ma,与伊列克得组玄武岩(125±2Ma)时代一致,两者构成了双峰式火山岩组合,形成于早白垩世岩石圈拉张环境。  相似文献   

Unusual rocks and mineralisation in a new carbonatite complex at Kandaguba, Kola Peninsula, Russia     

A. N. Pilipiuk  V. V. Ivanikov  A. G. Bulakh 《Lithos》2001,56(4):333-347

The paper presents the results from a reconnaissance investigation of carbonatites in a newly discovered alkaline complex in the Kola peninsula, Russia. The Kandaguba complex differs from other carbonatite plutons of the Kola alkaline province by (a) the absence of ultrabasic rocks, (b) widespread occurrence of nepheline-, cancrinite- and nepheline–cancrinite syenites and carbonatites and (c) presence of apatite–calcite ijolites and feldspar ijolites as separate intrusive phase. The Kandaguba carbonatites are notable for the predominance of late ferromagnesian varieties together with quartz and numerous accessory mineral species. The association of phosphates (monazite, gorseixite, goyazite, apatite), sulphides and tellurides (pyrite, sphalerite, galena, hessite), ilmenorutile, barite with quartz and ankerite is a remarkable feature of these carbonatites. The Kandaguba carbonatites are inferred to have been generated as the products of liquid immiscibility followed by differentiation of the carbonatite melt.  相似文献   

试论钾、钠、锂碱性元素在金银矿化异常评价及隐伏矿预测方面的应用──以山门银矿为例     

康太翰  于洪顺 《吉林地质》1995,(4)

本文以山门银矿床为例，研究和分析了碱性元素在矿化带三度空间上的含量变化和金银各侵蚀截面上异常变化特征。并建立碱性元素在金银矿床交代岩垂直分带综合模式。在此基础上进行了外围深部隐伏矿预测。  相似文献   

西秦岭月照-琵琶寺地区火山岩地球化学特征及地质意义     

刘军锋  孙勇  高明  杨磊 《地质学报》2008,82(7)

月照-琵琶寺地区的变质火山岩出露于甘肃武都县境内,夹在泥盆系和前震旦碧口群地层之间.按地球化学分类,火山岩可划分为双峰式和碱性两个系列.双峰式火山岩系由低K富Na拉斑玄武岩和酸性英安岩、流纹岩组成.该玄武岩具有类似MORB的微量元素特征,平坦的稀土配分模式,但富Th贫Nb显示其受到陆壳混染的影响.该套火山岩总体特征指示其为大陆裂谷向成熟洋盆转化阶段的产物,从而推测本区火山岩可能为勉略古洋盆西延的分支产物.  相似文献   

Petrogenesis of the Neogene alkaline volcanics with implications for post-collisional lithospheric thinning of the Eastern Pontides, NE Turkey   总被引：2，自引：0，他引：2  

Faruk Aydin  Orhan Karsli  Bin Chen 《Lithos》2008,104(1-4):249-266

Whole-rock geochemistry, Sr–Nd–Pb isotopes and K–Ar data are reported for alkaline samples collected from the Neogene alkaline volcanics (NAVs) in the Eastern Pontides, northeastern Turkey, in order to investigate their source and petrogenesis and geodynamic evaluation of the region. The NAVs were made of three groups that comprise of basanite–tephrite (feldspar-free; Group A), tephrite–tephriphonolite (feldspar and feldspathoid-bearing; Group B) and alkaline basalt–rhyolite (feldspathoid-free; Group C) series. These rocks cover a broad compositional range from silica-undersaturated to silica-oversaturated types, almost all of which are potassic in character. They show enrichment of LREE and LILE and depletion of HFSE, without a Eu anomaly in most of the mafic samples. Textural features and calculated pressures based on the Cpx-barometer in each series indicate that the alkaline magma equilibrated at shallow crustal depths under a pressure of about 3–4.5 kbar and approximating a crystallization depth of 9–14 km. The NAVs are slightly depleted in isotopic composition, with respect to ⁸⁷Sr/⁸⁶Sr (ranging from 0.705018 to 0.705643) and ¹⁴³Nd/¹⁴⁴Nd (ranging from 0.512662 to 0.512714) that indicate young Nd model ages (0.51–059 Ga). This may indicate that the parent melts tapped a homogeneous and young lithospheric mantle source which was metasomatized by subduction-derived sediments during the Late Mesozoic. Pb isotopic compositions (²⁰⁶Pb/²⁰⁴Pb = 18.85–18.95; ²⁰⁷Pb/²⁰⁴Pb = 15.60–15.74; ²⁰⁸Pb/²⁰⁴Pb = 38.82–39.25) may also be consistent with a model for an enriched subcontinental lithospheric mantle source. Lithospheric thinning and resultant upwelling of asthenosphere induced by lithospheric delamination may have favoured partial melting of chemically enriched, young lithospheric mantle beneath the Eastern Pontides. Then, the melt subsequently underwent a fractional crystallization process along with or without minor amounts of crustal assimilation, generating a wide variety of rock types in a post-collision extensional regime in the Eastern Pontides during the Neogene.  相似文献   

巴尔哲超大型稀有稀土矿床富晶体的流体包裹体初步研究   总被引：4，自引：2，他引：2  

牛贺才  单强  罗勇  杨武斌  于学元 《岩石学报》2008,24(9):2149-2154

巴尔哲矿床是一个超大型稀有稀土多金属矿床,它受巴尔哲碱性花岗岩体（株）控制,稀有稀土矿体分布在巴尔哲岩体上部的钠长石碱性花岗岩中。本文在钠长石碱性花岗岩的石英中发现了大量的富晶体的流体包裹体,并对其进行了初步的激光拉曼光谱和显微测温研究。与一般含盐类晶体矿物的三相流体包裹体不同,巴尔哲富晶体的流体包裹体的晶体不是盐类矿物,而是长石、云母等硅酸盐矿物;同时,该类包裹体内还广泛分布着稀土碳酸盐矿物。富晶体的流体包裹体的发现从微观角度揭示了巴尔哲含矿钠长石碱性花岗岩的形成与岩浆-热液过渡阶段有直接的成因联系,并为阐述巴尔哲岩体稀土元素及氧同位素的地球化学特征提供了新思路。稀土碳酸盐矿物在富晶体的流体包裹体中广泛地分布则充分说明。巴尔哲碱性花岗岩演化到岩浆-热液过渡阶段体系内的稀土元素已经达到足以形成独立稀土矿物的富集程度,其稀土元素矿化受岩浆-热液过渡阶段的制约。  相似文献   

朝鲜半岛北部定州与铁山稀土矿相关碱性岩和花岗岩的岩石学和SIMS锆石U-Pb年代学特征研究   总被引：2，自引：2，他引：0  

金正男  韩龙渊  赵磊  李秋立  金石山 《岩石学报》2016,32(10):3123-3138

朝鲜半岛北侧的狼林地块是中朝克拉通的重要组成部分,狼林地块具有与辽南地块以及辽吉活动带类似的早前寒武纪岩石组成、变质和变形特征。我们在分布有稀土矿的朝鲜定州-铁山一带(狼林地块西北部),采集了与稀土矿密切相关的碱性岩(粗粒正长岩和萤石化霓辉正长岩)和花岗岩(似斑状花岗岩)样品。岩石样品的岩相学观察表明,定州与铁山地区的碱性岩和花岗岩并不显示明显的岩浆期之后的热液蚀变特征。SIMS锆石U-Pb定年结果显示粗粒正长岩的岩浆结晶年龄为1865±6Ma,萤石化霓辉正长岩的岩浆结晶年龄为1868±8Ma,铁山地区的四件似斑状花岗岩的年龄结果分别为1871±13 Ma、1866±8 Ma、1872±6 Ma和1873±7 Ma,这些年龄值一方面代表了岩浆活动时代,另一方面可能也代表了朝鲜定州和铁山稀土矿的成矿时代。狼林地块的这些碱性岩与花岗岩的时代与华北克拉通辽吉活动带以及狼林地块其它地区的高级变质作用同期,并且在辽南地块,也有类似碱性岩的报道。综合现有的证据表明,辽吉活动带、辽南地块以及狼林地块在古元古代可能属于同一个大型构造带,并且这个构造带(或者构造带的一部分)当时处于伸展的构造背景。通过全面对比野外观测结果、岩石的岩相结构、岩浆结晶时代可知,朝鲜定州和铁山一带的稀土矿与中朝克拉通的世界级稀土矿——白云鄂博,在岩石组合、稀土矿物组成、岩石蚀变特征、成矿时代等方面存在较大的区别。关于这一稀土矿的具体稀土矿物组成、矿床成因以及储量等众多问题,未来还需要进行大量的工作。  相似文献   

Alkali-calcic and alkaline post-orogenic (PO) granite magmatism: petrologic constraints and geodynamic settings   总被引：30，自引：0，他引：30  

Bernard Bonin  Abla Azzouni-Sekkal  Franois Bussy  Sandrine Ferrag 《Lithos》1998,45(1-4):45-70

The end of an orogenic Wilson cycle corresponds to amalgamation of terranes into a Pangaea and is marked by widespread magmatism dominated by granitoids. The post-collision event starts with magmatic processes still influenced by subducted crustal materials. The dominantly calc-alkaline suites show a shift from normal to high-K to very high-K associations. Source regions are composed of depleted and later enriched orogenic subcontinental lithospheric mantle, affected by dehydration melting and generating more and more K- and LILE-rich magmas. In the vicinity of intra-crustal magma chambers, anatexis by incongruent melting of hydrous minerals may generate peraluminous granitoids bearing mafic enclaves. The post-collision event ends with emplacement of bimodal post-orogenic (PO) suites along transcurrent fault zones. Two suites are defined, (i) the alkali-calcic monzonite–monzogranite–syenogranite–alkali feldspar granite association characterised by [biotite+plagioclase] fractionation and moderate [LILE+HFSE] enrichments and (ii) the alkaline monzonite–syenite–alkali feldspar granite association characterised by [amphibole+alkali feldspar] fractionation and displaying two evolutionary trends, one peralkaline with sodic mafic mineralogy and higher enrichments in HFSE than in LILE, and the other aluminous biotite-bearing marked by HFSE depletion relative to LILE due to accessory mineral precipitation. Alkali-calcic and alkaline suites differ essentially in the amounts of water present within intra-crustal magma chambers, promoting crystallisation of various mineral assemblages. The ultimate enriched and not depleted mantle source is identical for the two PO suites. The more primitive LILE and HFSE-rich source rapidly replaces the older orogenic mantle source during lithosphere delamination and becomes progressively the thermal boundary layer of the new lithosphere. Present rock compositions are a mixture of major mantle contribution and various crustal components carried by F-rich aqueous fluids circulating within convective cells created around magma chambers. In favourable areas, PO suites pre-date a new orogenic Wilson cycle.  相似文献   

VC对河蟹血清和组织中超氧化物歧化酶及磷酸酶活性的影响   总被引：36，自引：2，他引：36  

艾春香  陈立侨  高露姣  温小波  江洪波 《台湾海峡》2002,21(4):431-438

研究了饲料中添加不同含量VC 对河蟹体内超氧化物歧化酶 (SOD)、碱性磷酸酶 (ALP)和酸性磷酸酶 (ACP)活性的影响 .结果表明 ,饲料中不添加VC 时 ,河蟹肝胰腺、卵巢、血清和肌肉各组织中SOD、ALP和ACP活性各异 ,其中SOD活性大小顺序为肝胰腺 >卵巢 >血清 >肌肉 ,ALP活性顺序为肝胰腺 >血清 >卵巢 >肌肉 ,而ACP活性则为肝胰腺 >血清 >肌肉 >卵巢 .饲料中VC 添加量分别 2 .5× 1 0 - 3 、5.0×1 0 - 3 、1 0 .0× 1 0 - 3 和 1 5.0× 1 0 - 3 (m m)时 ,与对照组相比 ,河蟹不同组织中SOD活性显著下降 (p <0 .0 5或 p <0 .0 1 ) ,而ALP、ACP这两种酶的活性却显著升高 (p <0 .0 5或 p <0 .0 1 ) .但它们的变化幅度不同 ,其中就肝胰腺、卵巢、血清和肌肉中SOD活性而言 ,VC 添加量为 1 5.0× 1 0 - 3 (m m )饲料组分别比对照组的低1 41 .3 4 %、1 2 5.94%、1 1 6.67%和 1 1 5.79%;ALP活性 ,VC 添加量为 1 0 .0× 1 0 - 3(m m)饲料组分别比对照组高 93 .0 %、77.5%、1 66.3 %和 2 66.4%;ACP活性 ,VC的添加量为 1 5.0× 1 0 - 3 (m m)饲料组分别比对照组高 1 3 0 .7%、2 3 7.4%、43 7.6%和 2 65.5%.饲料中VC 添加量为 (5.0～ 1 0 .0 )× 1 0 - 3 (m m )时 ,可有效地增强河蟹非特异性免疫能力 .此外 ,本实验还就VC  相似文献   

中华绒螯蟹精子形成过程酸性磷酸酶的分布特征     

刘桂荣  康现江  郭明申  孙文佳  王琦 《海洋通报(英文版)》2007,9(1):13-19

将金属盐法与光镜、电镜技术相结合,研究中华绒螯蟹精子形成过程中酸性磷酸酶分布的变化。研究表明,在精子形成的早期,酸性磷酸酶由细胞质中的内质网小泡上产生,随后出现在细胞核内、顶体囊膜上及顶体管内,并且反应产物逐渐由分布均匀的细密颗粒聚集成分布均匀的较大的颗粒;当精子成熟后酸性磷酸酶均匀分布在顶体管中,反应产物颗粒比较大,穿孔器部分发现有少量酸性磷酸酶分布。  相似文献