Decoupling of surface and subsurface sutures in the Dabie orogen and a continent-collisional lithospheric-wedging model：Sr-Nd-Pb isotopic evidences of Mesozoic igneous rocks in eastern China

Based on the distribution of UHPM rocks on the surface in Sulu terrane, the surface suture between the NCB and SCB should be located along the Wulian fault (see Fig. 1, S1). However, based on the aeromagnetic data of eastern China, Li[1] first indicated that the subsurface suture between the NCB and SCB in the region east of the Tan-Lu fault should be located to the east of Nanjing City (see Fig. 1, S2), which south displaced about 400 km from the surface suture. This is contradicto…     

三岔口火成岩特征及其与软玉成矿的关系

青海省东昆仑三岔口软玉矿区内出露的火成岩主要为基性辉长岩,地球化学分析显示稀土总含量高,强不相容元素、轻稀土元素富集,岩浆分异演化显著.构造投影判别及稀土、微量元素分配型式均反映了消减带火山弧环境.研究认为岩体为软玉的形成提供了Si和OH-等矿源物质,结合实地勘查资料提出该地软玉是在地壳深部还原性环境及较高的温度下,岩浆热液交代碳酸盐岩形成含软玉质热液,最终充填碳酸盐岩岩石裂隙而成.     

Isotopic composition of helium in eclogite from the Dabie Mountains, central China and its geological significance

Isotopic geochemical characteristics of helium in garnet and omphacite of eclogite in the Dabie Mountains are discussed. Concentrations of³He and⁴He in garnet and omphacite are 3.9 × 10⁻¹⁴–24.0 × 10⁻¹⁴ and 0.48 × 10⁻⁷–9.42 × 10⁻⁷cm¹³.g⁻¹, respectively. Values of³He/⁴He have a range of (1.19–4.63) × 10⁻⁷. Helium In the eclogite is derived from both mantle and crust. Isotopic geochemical data of helium indicate that eclogite in the Dabie Mountains might be formed in depleted mantle and the age of the cologite would be Indo-China epoch.     

江南元古宙古岛弧基底变质岩的Sm—Nd同位素研究

江南元古宙古岛弧的基底变质岩主要由浅变质的岛弧火山-沉积岩系组成。根据Sm-Nd同位素年龄资料,古岛弧西段基底变质岩的形成时间为早元古宙,中段为中元古宙中-晚期,东段为晚元古宙早期,形成时间持续长达13亿年左右。在9亿年前左右,江南古岛弧与华夏古陆发生碰撞拼贴,从而结束了江南古岛弧的演化史。     

基于BP网络的火成岩岩石化学分类研究

叙述了现有的火成岩分类方案中存在的诸如某些岩类在分类图解上没有空间,岩类因控制参数少存在投影重叠,岩石中存在同质异矿现象颗粒大小的极端差异以及含有玻璃质导致一些岩石分类错误等问题。提出了以BP网络算法为基础,以火成碉的SiO2,TiO2,Al2O3,FeO,MnO,MgO,CaO,Na2O,K2O,P2O5等11个氧化物成分变量,使用人工神经网络建立火成岩岩石化学分类模型。研究表明,该分类方法是合理的,可行的,取得了良好的分类效果;对训练对样本的判对率为92．18％,而对46个检验样本的判对率达97．8％。     

Rutile U-Pb age for the ultra-high pressure eclogite from the dabie Mountains,central China:Evideence for rapid cooling

The U-Pb isotope compositions of rutile, omphacite and garnet in the eclogite from the Jinheqiao area in the Southern Dabie ultrahigh-pressure metamorphic zone were analyzed. The consistent high precision U-Pb age (218 ±(1.2) Ma of rutile in eclogite from the Dabie Mountains was obtained by two ways of isochron and common Pb correction based on the composition of omphacite. This proves that the omphacite in eclogite has a U/Pb ratio (μ = 2.8) low enough to be used for common Pb correction in the analyses of rutile. Under the rapid cooling condition (40℃/Ma) the closure temperature for U-Pb diffusion in rutile is about 470℃. Thus, this U-Pb age of rutile proves that 218 Ma should be the cooling age of eclogite at 470℃ instead of the peak metamorphic age.     

大别山革命根据地与全国解放战争

大别山革命根据地是中国共产党领导革命战争的重要战略基地。在解放战争时期,大别山革命根据地在人民解放战争中发挥了极其重要的作用,在战略防御阶段,它是抵御国民党军对解放区全面进攻的前哨阵地,在战略进攻阶段,它又是人民解放军战略进攻的前哨和尖兵。以大别山革命根据地为中心的中原解放区是夺取全国解放战争胜利的前进基地。大别山根据地和大别山人民为中国新民主主义革命的胜利建立了卓著的功勋。     

扬子陆块西北缘拉伸纪三期岩浆作用对Rodinia超大陆裂解的指示意义

为了解扬子陆块西北缘新元古代拉伸纪(1 000~720 Ma)岩浆活动和构造演化历史,该文统计了扬子陆块北东缘至西南缘45个岩浆岩岩体的全岩元素、Sm-Nd同位素、锆石U-Pb年龄及Hf同位素数据。根据岩石组合和地球化学特征,可以将扬子西北缘拉伸纪岩浆活动划分为3个阶段,早于855 Ma、855~770 Ma和晚于770 Ma。通过统计和对比3个阶段岩浆岩地球化学特点认为,扬子西北缘洋壳俯冲和岛弧岩浆侵位在1 000~900 Ma进入停止期,在900~855 Ma开始进入长期弧陆碰撞和增生造山向碰撞后伸展阶段,至830 Ma之后,扬子陆块边缘进入到全面的大陆裂谷背景,并伴有与Rodinia超大陆裂解有关的岩浆作用。     

峨眉山大火成岩省内带中酸性岩浆岩对地幔柱岩浆过程及地壳熔融机制的启示

峨眉山大火成岩省内带攀西地区分布大量晚二叠世中酸性岩浆岩,其成因机制对深化理解地幔柱岩浆作用过程、壳幔物质结构及特殊的金属元素成矿作用具有重要意义。这些中酸性岩浆岩包括中性碱性岩和花岗岩,形成时代集中于251~259 Ma左右,稍晚于峨眉山溢流玄武岩的形成时代(~260 Ma)。目前,对于这套中酸性岩浆岩的成因还存在争议,主要有玄武质岩浆的结晶分异和地壳物质的高温部分熔融两种观点。文中对峨眉山大火成岩省内带这套中酸性岩浆岩的岩石组成、空间展布、形成时代及成因机制等方面的研究进展进行了详细评述,提出对这套中酸性岩浆岩高精度年代学的研究可以进一步约束峨眉山地幔柱岩浆作用的时限。而从矿物化学的角度,深入研究这套中酸性岩浆岩的成因,不仅是对地幔柱岩浆过程的重要补充,同时对深入研究地幔柱背景下岩石圈地幔和地壳物质的分异及增生机制有重要意义。