Subsolidus Phase Relations in the System MgO-SiO_2-Cr-O and Thermodynamic Properties of Related Cr~(2+)-Containing End-members

Subsolidus phase relations have been determined in the systems SiO2-Cr-O and MgO-SiO2-Cr-O in equilibrium with metallic Cr, at 1100 to 1500℃ and 0 to 2.88 GPa. The results show that there are no ternary phases in the SiO2-Cr-O system at these conditions, i.e., only the assemblage eskolaite-Cr-metal-quartz (or tridymite) is found. In the MgO-containing system, however, extensive substitution of Cr2+ for Mg is observed in (Mg, Cr2+)2SiO4 olivine, (Mg, Cr2+)2Si2O6 pyroxene, and (Mg, Cr2+)Cr2O4 spinel. Cr3+ levels in olivine and pyroxene are below detection limits. The pyroxene is orthohombic at XCrPx2+ < 0.2, monoclinic at higher XCrPx2+ . Thestructure of the spinels becomes tetragonally distorted at XCr2+Sp >0.2. The experimental datahave been fitted to a thermodynamic model, and the authors obtained the mixing parameter (W) of Mg-Cr2+ in olivine, pyroxene and spinel, and the relation between temperatures and free energies of formation for the end-members: Cr2+-olivine (Cr2SiO4), Cr2+-pyroxene (Cr2Si2O6)     

湘西沃溪金锑钨矿床黄铁矿矿物学研究

本结合矿床地质背景，从时间空间分布，晶体形态，化学成分（包括主成分，微量元素，元素对比值，元素组合等）晶胞参数，热电性，反射光谱等方面对黄铁矿进行比较详细的研究，确定了本矿床黄铁矿在上述诸方面的标型特征，为指导找矿勘探提供了重要的理论依据。     

秦巴北部商县—卢氏地区变质方解石—白云石地质压力计的研究

秦巴北部的商县-卢氏县地区广泛分布有区域变质的方解石-白云石共生矿物对,它们对于估计变质作用和断裂构造作用的温压条件,有着重要的意义。本文着重就该地区Fe~(2+)在方解石-白云石中的X_(Fe)~(Co)>X_(Fe)~(Dol)分配情况,提出新的计压方法。     

山东金伯利岩中的钛钡铬石—钛钾铬石系列

山东金伯利岩中的副矿物钛钡铬石、钛钾铬石在我国属首次发现,它们是锶钛铁矿族一个类质同象系列的大阳离子分别以Ba和K为主的两种新矿物。本文通过化学成分、穆斯堡尔谱、反射光谱、X射线粉晶衍射等分析研究,为这两种矿物提供了有意义的矿物学资料。     

Chemostratigraphy of Flood Basalts in the Garze-Litang Region and Zongza Block: Implications for Western Extension of the Emeishan Large Igneous Province, SW China

The Late Permian Emeishan Large Igneous Province (ELIP) is commonly regarded as being located in the western part of the Yangtze craton, SW China, with an asymmetrical shape and a small area. This area, however, is just a maximum estimation because some parts of the ELIP were not recognized or dismembered and destroyed during the Triassic to Cenozoic tectonism. In this paper, the chemostratigraphical data of the Zongza block, the Garze-Litang belt and the Songpan-Garze block suggest that the Late Permian basalts in these areas have remarkable similarities to the ELIP basalts in petrography and geochemistry. Flood basalts in the Sanjiangkou area are composed of the lower part of the low-Ti (LT) tholeiite and the upper part of the high-Ti (HT) tholeiite, which is the same as the flood basalts on the western margin of the Yangtze craton. Flood basalts in the Zongza and Songpan-Garze areas, which are far from the Yangtze craton, consist of HT tholeiite only. This is the same as the flood basalts within the Y     

柴达木盆地茫崖坳陷古近系—新近系R_o分布特征及地质意义

柴达木盆地西部的茫崖坳陷是青海油田的主力油气产区 ,对该区古近系—新近系镜质组反射率(Ro)进行了系统研究 ,发现其垂向分布有两种规律 :一是 Ro 与垂深有良好的线性关系 ,多分布在坳陷中央 ,反映了沉积环境、物源和构造的稳定性较好 ;二是 Ro 与垂深呈右阶状 ,反映了逆冲叠覆。此外 ,通过 EASY% Ro 方法计算了研究区地层剥蚀厚度 ,认为干柴沟—油泉子为英雄岭隆起的主轴 ,因为剥蚀了 36 0 0～ 375 0 m,所以英雄岭主峰在地形上呈现出隆起主轴的假貌。通过地层剥蚀厚度的研究 ,还发现油气田主要分布在剥蚀梯度带上。这一结论对柴达木盆地油气勘探开发具有重要意义     

南天山库车秋里塔格褶皱带三维构造分析

笔者利用库车秋里塔格地区3000km的二维地震反射资料，结合地表构造测量成果，分段叙述秋里塔格褶皱带的构造几何学和运动学性质，说明构造交汇部位断层和褶皱的叠加过渡关系，并通过二维构造剖面的组合，建立秋里塔格褶皱带的三维构造几何模型。研究发现秋里塔格褶皱带为浅部断层传播褶皱与深部断层转折褶皱叠加形成的复合型背斜带，深部台阶状逆断层的叠加作用、叠加断层位移量的转换、断层断坡高度的变化造成地表背斜沿走向发生变化，笔者通过测量断层叠加方式、断层位移量转换、断层断坡高度，说明秋里塔格褶皱带背斜叠加、扭曲、分叉现象的构造机理，并且给出了秋里塔格褶皱带断层的滑移量。     

青藏高原东缘古近纪粗碎屑岩沉积学及其构造意义

青藏高原东缘古近纪盆地的填图和沉积学研究表明,在青藏高原东缘区域性走滑-挤压构造背景下形成的古近纪盆地内广泛发育厚层—巨厚层状的紫红色粗碎屑岩系。其沉积特征指示为一种近源快速堆积的泥石流和辫状河道沉积体,形成于干旱炎热气候条件下的典型陆内冲积扇环境。盆地充填序列、粗碎屑岩层序、动植物化石和盆地内岩浆岩~(40)Ar-~(39)Ar年代学等综合研究结果表明,古近纪盆地内粗碎屑岩大约形成于38～29 Ma。该时期与青藏高原东缘北段(横断山地区)古近纪盆地的形成和南段(兰坪—思茅地区)大盆地的裂解时间基本一致,这很可能预示着青藏高原在晚始新世—早渐新世期间曾发生过整体的快速构造隆升。     

三套管(NQ3)取心钻进工艺原理及在60°斜孔施工中的应用

为矿产勘察开发提出完整可靠的选矿验证,资源量验证及岩土力学原始资料,引进三套管(NQ3)取心工艺并进行了应用试验,重点介绍了该工艺的原理以及在金矿勘查60°斜孔施工中的应用.     

两类埃达克岩(Adakite)的判别

埃达克岩是目前地学界的研究热点 ,普遍认为具有两种成因类型。在大量分析已经发表的两类埃达克岩资料的基础上 ,发现通过 Sr/Y- w (Y)散点图、Sr- Y× 10 - Zr三角图、Y/Yb- Sr/Y- L a/Yb三角图能够判别 , 类埃达克岩。