哀牢山墨江金矿与南乌拉尔山明加克金矿地质特征对策   总被引：1，自引：0，他引：1  

李光明  刘铁兵等 《矿物学报》2001,21(4):631-638

本文通过对产于两个不同造山带中金矿化特征的对比，认为墨江金矿与明加克金矿均具有造山带型金矿的一些特征，形成于造山晚期主构造带的逆冲走滑阶段，产于一级构造带的上盘，金矿化受二级和三级剪切张裂隙的控制。与明加克金矿不同的是墨江金矿的形成经历了更长的构造演化历史。  相似文献   

Ground-Space Correlation of TM Data and Its Application to the Prediction of Gold Deposits     

WANG Haiping  HU Yunzhong  Institute of Mineral Deposits  Chinese Academy of Geological Sciences  Beijing ZHANG Zonggui  CHEN WeiCentre of Aerogeophysical Prospecting  Remote Sensing  Ministry of Geology  Mineral Resources  Beijing Jiang Ruiliang 《《地质学报》英文版》1998,72(2):142-153

It has been inferred and proved by the remote sensing equations under rational hypotheses in atmospheric physics that there is a linear correlation between the ground reflective brightness Wij and the total reflective brightness Rij received in different bands with a remote sensor. Nine models delineating the ground-space correlation between the ground spectra and the optimal bands of images of the typical gold deposits have been established based on the ground-space correlativity and field measurements of the ground spectra of the typical gold deposits in the Ailaoshan area. According to the 9 correlation models, TM images were inverted into ground-space correlation images that are related to the typical gold deposits within the area and then recognized by a computer. Research on the ground . spectra and TM data in the Ailaoshan area shows that the correlation analysis of the ground spectra and TM data of gold deposits can be effectively applied to the prediction of gold deposits, location of prospecti  相似文献   

The Jinshajiang–Ailaoshan Suture Zone, China: tectonostratigraphy, age and evolution     

Xiaofeng Wang  I. Metcalfe  Ping Jian  Longqing He  Chuanshan Wang 《Journal of Asian Earth Sciences》2000,18(6):160

The Jinshajiang Suture Zone is important for enhancing our understanding of the evolution of the Paleo-Tethys and its age, tectonic setting and relationship to the Ailaoshan Suture Zone have long been controversial. Based on integrated tectonic, biostratigraphic, chemostratigraphic and isotope geochronological studies, four tectono-stratigraphic units can be recognized in the Jinshajiang Suture Zone: the Eaqing Complex, the Jinshajiang Ophiolitic Melange, the Gajinxueshan “Group” and the Zhongxinrong “Group”. Isotope geochronology indicates that the redefined Eaqing Complex, composed of high-grade-metamorphic rocks, might represent the metamorphic basement of the Jinshajiang area or a remnant micro-continental fragment. Eaqing Complex protolith rocks are pre-Devonian and probably of Early–Middle Proterozoic age and are correlated with those of the Ailaoshan Complex. Two zircon U–Pb ages of 340±3 and 294±3 Ma, separately dated from the Shusong and Xuitui plagiogranites within the ophiolitic assemblage, indicate that the Jinshajiang oceanic lithosphere formed in latest Devonian to earliest Carboniferous times. The oceanic lithosphere was formed in association with the opening and spreading of the Jinshajiang oceanic basin, and was contiguous and equivalent to the Ailaoshan oceanic lithosphere preserved in the Shuanggou Ophiolitic Melange in the Ailaoshan Suture Zone; the latter yielded a U–Pb age of 362±41 Ma from plagiogranite. The re-defined Gajinxueshan and Zhongxinrong “groups” are dated as Carboniferous to Permian, and latest Permian to Middle Triassic respectively, on the basis of fossils and U–Pb dating of basic volcanic interbeds. The Gajinxueshan “Group” formed in bathyal slope to neritic shelf environments, and the Zhongxinrong “Group” as bathyal to abyssal turbidites in the Jinshajiang–Ailaoshan back-arc basin. Latest Permian–earliest Middle Triassic synorogenic granitoids, with ages of 238±18 and 227±5–255±8 Ma, respectively, and an Upper Triassic overlap molasse sequence, indicate a Middle Triassic age for the Jinshajiang–Ailaoshan Suture, formed by collision of the Changdu-Simao Block with South China.  相似文献   

哀牢山南段长安金矿床成矿流体特征及成因类型探讨   总被引：5，自引：5，他引：0  

李士辉  张静  邓军  王欢  刘江涛  赵凯 《岩石学报》2011,27(12):3777-3786

长安金矿床是三江造山带哀牢山成矿带南段大型矿床之一,就位于甘河断裂的脆性破碎带内.其成矿流体具有中低温、中低盐度的特点,气相成分以H2O、CO2为主,主成矿期流体中CO2含量可达21.162mo1％～32.832mo1％;液相成分以Cl-、K+、Na+为主.成矿流体的δ13CCo2值为-3.427‰～8.749‰,显示海相碳酸盐源特征并与岩浆活动有关;δD值为-111‰～ -78.383‰,δ18O值介于10.527‰～13.565‰,δ34S值集中分布在+1‰～+3‰之间,综合表明长安金矿流体具有岩浆热液的性质,同时,源自海相碳酸盐地层的变质水也参与了成矿作用.在哀牢山南段的金平地区,受新生代大规模富碱性岩浆沿断裂上侵的影响,含金的岩浆气液在运动过程中混合浅部流体并活化、萃取矿区地层及有关地质体中的金元素,使其转入溶液形成含金的成矿流体;当成矿流体运移到浅部有利构造或岩性部位时,物理化学条件的变化,促使Au等成矿物质快速沉淀、富集形成微细浸染状矿化.综合研究认为,长安金矿床兼具造山型和卡林型金矿床的典型地质地球化学特征,可被厘定为类卡林型金矿床,为卡林型与造山型之间的过渡类型.  相似文献   

Two‐Stage Sulfide Mineral Assemblages in the Mineralized Ultramafic Rocks of the Laowangzhai Gold Deposit (Yunnan,SW China): Implications for Metallogenic Evolution     

Huichao Zhang  Peng Chai  Hongrui Zhang  Zengqian Hou  Shouming Chen  Yanbin Sun  Qing Peng 《Resource Geology》2019,69(3):270-286

The Laowangzhai gold deposit, located in the Ailaoshan gold belt (SW China), is hosted in various types of rocks, including in quartz porphyry, carbonaceous slate, meta‐sandstone, lamprophyre, and altered ultramafic rocks. In contrast to other wall rocks, the orebodies in altered ultramafic rocks are characterized by the occurrence of a large amount of Ni‐bearing minerals. The ore‐forming process of the orebodies hosted by altered ultramafic rocks can be divided into two stages: pyrite‐vaesite‐native gold and gersdorffite‐violarite stages. The contents of As and Sb increased during the evolution of ore‐forming fluid based on the mineral assemblages. Thermodynamic modeling of the Ni‐Cu‐As‐Fe‐S system using the SUPCRT92 software package with the updated database of slop16.dat indicates the fS₂ in ore‐forming fluid decreases significantly from stage I to stage II. The decreases of fS₂ due to crystallization of sulfides and fO₂ due to fluid–rock reaction were responsible for ore formation in altered ultramafic rocks of the Laowangzhai gold deposit. Geological evidence, the in situ sulfur isotope values of pyrite, and the other published isotopic data suggest that the ore‐forming fluid for ultramafic rock ores was dominantly composed of evolved magmatic fluid with the important input of sediments.  相似文献   

哀牢山古特提斯洋缝合时限：晚二叠世花岗岩类锆石U-Pb年代学与地球化学制约   总被引：18，自引：16，他引：2  

李龚健  王庆飞  禹丽  胡兆初  马楠  黄钰涵 《岩石学报》2013,29(11):3883-3900

金沙江-哀牢山缝合带系三江特提斯构造域东缘一条重要古特提斯缝合带,其南段哀牢山缝合带闭合的时限及其岩浆活动响应,尚缺乏精确的年代学与岩石地球化学制约。本文对出露于哀牢山缝合带北部老王寨矿区的花岗岩类进行了锆石U-Pb年代学、Hf同位素与全岩微量元素地球化学研究。2件花岗斑岩(D12-1与D13-1)²⁰⁶Pb/²³⁸U加权平均年龄为247.7±1.8Ma与255.0~251.7Ma,1件石英斑岩(L12-8)为255.1±3.4Ma,表明一次晚二叠世的岩浆事件。微量元素地化结果显示清晰的Rb、U、Th、Pb正异常和Ba、Sr、Ti、Nb负异常以及轻重稀土强烈分异(LREE/HREE=7.2~18.2)与负Eu异常(0.74~0.78)特征,结合前人主量元素分析表现出的过铝质与高钾钙碱质结果,认为其主体系加厚地壳的富铝沉积岩区深熔形成的S型花岗岩。花岗斑岩ε_Hf(t)值总体集中于0.8~3.3,也含有少量异常正值(7.2)和负值(-5.1和-2.9),解释其源区为亏损地幔与地壳(沉积源区特征明显)的混合。石英斑岩ε_Hf(t)值分布很窄,结果均为负值(-5.5~-2.3),认为其可能系下地壳先存弧岩浆岩源区部分熔融的结果。花岗斑岩锆石较石英斑岩锆石显示重稀土元素分馏相对显著与Ti温度计结果偏高的特征,表现出与其源区中地幔组分的涉入作用相关。总体加厚地壳背景下成生的岩浆岩涉入地幔组分,反映岩浆活动发生于哀牢山缝合带的后碰撞伸展背景。综合新近发表的俯冲型与碰撞型岩浆岩锆石U-Pb定年数据,将哀牢山缝合带闭合的时间限定在晚二叠世(~260Ma),其早于西侧昌宁-孟连洋与北段金沙江洋闭合的时限(分别为中三叠世~235Ma和早三叠世~245Ma)。  相似文献   

High Temperature Strain Structures and Quartz C-Axis Fabrics from Mylonitic Rocks in the Ailaoshan-Red River Shear Zone, Yunnan, and Their Tectonic Implication   总被引：3，自引：0，他引：3  

LIU Junlai  TANG Yuan  XIA Haoran  GUO Qiang  TRAN My Dung  CAO Shuyun  WU Hujun  WU Wenbin  ZHANG Zhaochong  ZHAO Zhidan 《《地质学报》英文版》2010,84(6):1377-1390

<正>The Ailaoshan-Red River(ASRR) shear zone is one of the major Southeast Asian tectonic discontinuities that have figured the present tectonic framework of the eastern Tibet.Several metamorphic massifs are distributed linearly along the shear zone,e.g.Xuelongshan,Diancangshan, Ailaoshan and Day Nui Con Voi from north to south.They bear a lot of lines of evidence for the tectonic evolution of the eastern Tibetan at different crustal levels in different tectonic stages.Controversy still exists on the deformation structures,microstructures and their relationship with metamorphisms along the ASRR.In this paper detailed microstructural and EBSD(Electron Backscattered Diffraction) fabric analysis of some highly sheared granitic rocks from different massifs along the ASRR are conducted.High temperature structures and microstructures are preserved in unsheared gneisses,in weakly sheared xenoliths or in some parts of the highly sheared rocks(mylonites).Several types of high temperature quartz c-axis fabrics show symmetrical patterns or transitions from symmetrical to asymmetrical patterns.The former are attributed to coaxial deformation during regional shortening in an early stage of the Indian-Eurasian tectonic interaction and the latter are related to the transitions from coaxial compression to noncoaxial shearing during the post-collisional ASRR left lateral shearing.  相似文献   

云南哀牢山大坪金矿床成矿流体H-O-C-S同位素组成及其成矿意义   总被引：5，自引：4，他引：1  

石贵勇  孙晓明  张燕  熊德信  翟伟  潘伟坚  胡北铭 《岩石学报》2010,26(6):1751-1759

大坪金矿是云南哀牢山金矿带中最大的新生代造山型金矿之一,其矿体可分为两种类型:晚元古代闪长岩岩体中金矿和中泥盆统马鹿洞组(D2m)灰岩地层中金矿。成矿流体H-O-C-S同位素研究表明,闪长岩岩体中金矿δ18OH2O为2.39‰～7.59‰,δD为-85‰～-60‰,热液方解石的δ13C值为-4.7‰～-4.6‰,黄铁矿δ34S值为-2.8‰～7.6‰,平均3.1‰,方铅矿δ34S值为0.2‰～6.3‰,平均2.0‰,而灰岩地层中金矿的δ18OH2O值为4.36‰～6.82‰,δD为-75‰～-67‰,热液铁白云石和方解石δ13C为-7.6‰～-0.5‰,黄铁矿δ34S值为2.2‰～10.2‰,平均6.5‰,显示大坪金矿中两种主要金矿类型成矿流体的组成和来源基本一致,均主要为来自下地壳的变质流体组成,但有地幔流体加入。大坪金矿属于剪切带控制的中深中温热液型金矿,其成矿与哀牢山金矿带在喜马拉雅早期强烈的壳幔相互作用有关。来自下地壳和地幔的深源流体沿超壳剪切带上升,在地壳浅部向次级断裂构造流通,分别在闪长岩体和灰岩地层中成矿。围岩不是大坪金矿的主要控矿因素。  相似文献   

哀牢山工程地质问题及对策     

刘伟 《云南地质》2010,29(4):463-466

哀牢山地区工程地质及水文地质条件十分复杂:构造运动、斜坡地形、水文地质条件、地层岩性及高地热异常、高地应力的作用等"两高"、"四复杂",使哀牢山地区的工程地质条件十分困难。对工程方案及工程措施提出改进建议,确保穿越哀牢山区铁路等线状工程方案合理、措施得当。  相似文献   

Study on deep structure in Ailaoshan region based on aeromagnetic interpretations     

PENG Yuanyuan  LI Shichao    LU Laijun  LIU Guangsheng  WU Jun. College of Earth Sciences  Jilin University  Changchun  China 《东北亚地学研究》2009,(4):189-193

Linear and circular interpretation structure maps of different relative depths are obtained by processing 1：200000 aeromagnetic data to the pole in Ailaoshan region, interpreting upward extension of 4 heights, extracting a vertical second derivative line of 0 value and a series of calculations. Concealed boundary of deep magnetic rocks can be delineated according to the maps. On the basis of the conclusions above, a set of economical and practical methods to graph the deep structure are summarized. In addition, the relationship between deep structure and mineralization positions is discussed.  相似文献