云南武定刺竹箐铅锌矿矿床成因     

庄荣寿 《云南地质》2011,30(2):148-150

矿体赋存于主干断裂附近的次级构造裂隙中,分硫化矿和氧化矿,属热液充填型铅锌矿。  相似文献   

云南富宁安那金矿控矿因素分析   总被引：1，自引：0，他引：1  

寸伟才  王绍明  涂国府 《云南地质》2011,30(3):265-268

安那金矿赋存于中泥盆统坡折落组硅质岩夹薄层状灰岩中。东西向安那不对称褶皱构造是主要控岩控矿构造,次级北东向断裂和层间断裂是矿区的储（容）矿构造;矿区的金矿化与基性岩浆活动关系密切。  相似文献   

红河车古铁金多金属矿矿化特征及成因探讨     

孙玉海  李娜  坚润堂  柴旺  蹇龙  詹关山 《云南地质》2011,30(4):425-427

红河县车古铁多金属矿为近期新发现的金矿点,通过矿区已发现的三处矿化体的综合研究,并与典型矿床进行对比,认为本区金矿化体均为热液成因。  相似文献   

Effect of implementing ecosystem functional type data in a mesoscale climate model     

Seung-Jae LEE  E. Hugo BERBERY  Domingo ALCARAZ-SEGURA 《大气科学进展》2013,30(5):1373-1386

In this paper, we introduce a new concept of land-surface state representation for southern South America, which is based on "functional" attributes of vegetation, and implement a new land-cover (Ecosystem Functional Type, hereafter EFT) dataset in the Weather and Research Forecasting (WRF) model. We found that the EFT data enabled us to deal with functional attributes of vegetation and time-variant features more easily than the default land-cover data in the WRF. In order to explore the usefulness of the EFT data in simulations of surface and atmospheric variables, numerical simulations of the WRF model, using both the US Geological Survey (USGS) and the EFT data, were conducted over the La Plata Basin in South America for the austral spring of 1998 and compared with observations. Results showed that the model simulations were sensitive to the lower boundary conditions and that the use of the EFT data improved the climate simulation of 2-m temperature and precipitation, implying the need for this type of information to be included in numerical climate models.  相似文献   

太阳针状体的观测研究进展     

赵瑞娟  张宇宗  刘煜  田占军  赵明宇  徐稚  申远灯 《天文学进展》2014,(4)

针状体是太阳的基本结构,人们对它的研究已有100多年的历史,在观测和理论方面取得突破性进展。由于针状体本身的特点(小结构尺度、高动态、短寿命),对它的观测研究十分依赖望远镜的分辨率。文章主要描述借助于Hinode卫星搭载的SOT空间望远镜、SST(The Swedish1-m SolarTelescope,瑞典1 m太阳望远镜)等地基太阳望远镜所取得的关于色球针状体及其日面对应物的观测研究成果。主要包括以下几个方面:(1)针状体的形态,如轨迹、高度、长度、速度等,和由此而得到的分类;(2)针状体的日面对应物——纤维和日芒;(3)针状体的起源机制。即便今天,针状体仍然存在许多未解之谜:II型针状体是否存在?针状体和它日面对应物之间的关系是什么?如果存在两种类型的针状体,那么它们的激发机制是什么?它的波动是由什么引起?针状体能否加热日冕和加速太阳风?作为太阳的基本结构,在其他恒星上是否存在?等等。  相似文献   

小兴安岭平顶山一带早侏罗世花岗岩类年代学、地球化学特征及其地质意义     

尹志刚  宫兆民  王春生  刘松杰  张圣听  王冠群  周小刚  张志浩 《吉林大学学报(地球科学版)》2021,51(1):107-125

小兴安岭平顶山大地构造位于兴蒙造山带东段,隶属松嫩地块。本文对小兴安岭平顶山一带碱长花岗岩和正长花岗岩进行了锆石U-Pb年代学和岩石地球化学研究,以确定其形成时代、岩石成因及大地构造背景。结果显示：碱长花岗岩形成于（189±3） Ma,正长花岗岩形成于（191±3） Ma,同为早侏罗世岩浆事件演化的产物;岩石具有高硅（w（SiO₂）为75.00%~77.60%）、富碱（w（K₂O+Na₂O）为7.13%~9.00%）、贫镁（w（MgO）为0.05%~0.45%）、贫钙（w（CaO）为0.17%~1.10%）、低磷钛（w（P₂O₅）为0.01%~0.07%,w（TiO₂）为0.09%~0.23%）的特点,A/CNK值为0.94~1.17,属于准铝质-弱过铝质、高钾钙碱性系列岩石;亏损高场强元素Nb、P、Ti、Ta和大离子亲石元素Ba、Sr,Rb、K、Th、Hf等元素具有明显的正异常;稀土元素总量（w（ΣREE））为（38.76~297.13）×10^-6,稀土配分曲线显示为轻稀土略微富集、重稀土较为平坦缓向倾斜的右倾型,具明显的负Eu异常。锆石饱和温度值及地球化学特征等多种证据显示,岩石为高分异的I型花岗岩。结合小兴安岭区域构造演化特征分析,研究区早侏罗世花岗岩类为松嫩地块与佳木斯地块沿嘉荫—牡丹江缝合带碰撞拼合后伸展环境下的产物,岩浆起源于下地壳火成岩物质的部分熔融。  相似文献   

Evaluation of the petroleum composition and quality with increasing thermal maturity as simulated by hydrous pyrolysis: A case study using a Brazilian source rock with Type I kerogen     

《Organic Geochemistry》2015

Hydrous pyrolysis (HP) experiments were used to investigate the petroleum composition and quality of petroleum generated from a Brazilian lacustrine source rock containing Type I kerogen with increasing thermal maturity. The tested sample was of Aptian age from the Araripe Basin (NE-Brazil). The temperatures (280–360 °C) and times (12–132 h) employed in the experiments simulated petroleum generation and expulsion (i.e., oil window) prior to secondary gas generation from the cracking of oil. Results show that similar to other oil prone source rocks, kerogen initially decomposes in part to a polar rich bitumen, which decomposes in part to hydrocarbon rich oil. These two overall reactions overlap with one another and have been recognized in oil shale retorting and natural petroleum generation. During bitumen decomposition to oil, some of the bitumen is converted to pyrobitumen, which results in an increase in the apparent kerogen (i.e., insoluble carbon) content with increasing maturation.The petroleum composition and its quality (i.e., API gravity, gas/oil ratio, C₁₅₊ fractions, alkane distribution, and sulfur content) are affected by thermal maturation within the oil window. API gravity, C₁₅₊ fractions and gas/oil ratios generated by HP are similar to those of natural petroleum considered to be sourced from similar Brazilian lacustrine source rocks with Type I kerogen of Lower Cretaceous age. API gravity of the HP expelled oils shows a complex relationship with increasing thermal maturation that is most influenced by the expulsion of asphaltenes. C₁₅₊ fractions (i.e., saturates, aromatics, resins and asphaltenes) show that expelled oils and bitumen are compositionally separate organic phases with no overlap in composition. Gas/oil ratios (GOR) initially decrease from 508–131 m³/m³ during bitumen generation and remain essentially constant (81–84 m³/m³) to the end of oil generation. This constancy in GOR is different from the continuous increase through the oil window observed in anhydrous pyrolysis experiments. Alkane distributions of the HP expelled oils are similar to those of natural crude oils considered to be sourced from similar Brazilian lacustrine source rocks with Type I kerogen of Lower Cretaceous age. Isoprenoid and n-alkane ratios (i.e., pristane/n-C₁₇ and phytane/n-C₁₈) decrease with increasing thermal maturity as observed in natural crude oils. Pristane/phytane ratios remain constant with increasing thermal maturity through the oil window, with ratios being slightly higher in the expelled oils relative to those in the bitumen. Generated hydrocarbon gases are similar to natural gases associated with crude oils considered to be sourced from similar Brazilian lacustrine source rocks with Type I kerogen of Lower Cretaceous, with the exception of elevated ethane contents. The general overall agreement in composition of natural and hydrous pyrolysis petroleum of lacustrine source rocks observed in this study supports the utility of HP to better characterize petroleum systems and the effects of maturation and expulsion on petroleum composition and quality.  相似文献   

激电中梯测量在龙湾套铜矿找矿中的应用     

王继芳  王娜  黄坤朋 《云南地质》2014,(4):605-609

泗水县龙湾套铜矿为岩浆熔离型铜镍硫化物矿床,通过激电中梯测量圈定了若干激电异常,经工程验证,不但在这些异常中发现了9个铜矿体,而且各矿体的形态,规模与异常的形态,规模大致吻合.  相似文献   

云南富宁县牛场钛铁砂矿矿床成因及富集规律   总被引：1，自引：0，他引：1  

赵作新  沈辉  赵梓涵 《云南地质》2014,(4):520-525

富宁地区里达断裂东侧出露大量的中三叠世印支期第一期第四亚期侵入的辉长辉绿岩体,经过漫长的风化、水解作用,岩体岩石结构构造遭受破坏,钛铁矿、钛磁铁矿、金红石等矿石矿物从原岩中彻底解离,从而形成了易开采利用的辉长辉绿岩风化壳型钛铁矿（砂）矿床.  相似文献   

云南云县新村金矿床成因类型     

付奉甜  刘小春 《云南地质》2014,(1):123-126

金矿赋存于三叠系中统忙怀组上段第二层（T2m2-2）的蚀变安山岩的地层中,矿体受断层及火山岩双重控制,近矿围岩蚀变主要有硅化、黄（褐）铁矿化、毒砂化、方解石化等.认为该矿区金矿床成因类型为与火山作用、构造作用有关的蚀变岩型金矿床,并总结了矿区的找矿标志,对在该区域寻找该类型的金矿床具有一定的指导意义.  相似文献