柯坪露头区早志留世三角洲及碎屑海岸沉积   总被引：1，自引：1，他引：0       下载免费PDF全文

邢凤存  李祯 李思田 《中国地质》2011,38(4):996-1007

塔里木盆地阿克苏市柯坪露头区下志留统地层出露连续、完整,是较好的海相碎屑岩沉积露头研究区,其沉积体系类型有待进一步探讨。笔者通过多次精细的露头沉积学观察及室内研究,对柯坪露头区下志留统海相碎屑岩沉积体系类型及其特征进行了分析研究。识别出三角洲及碎屑海岸沉积(潮坪),并在该区提出了河流作用为主的三角洲和潮汐影响三角洲两种三角洲类型。柯坪塔格组主要为河流作用为主的三角洲沉积,而塔塔埃尔塔格组则主要发育潮汐影响三角洲及潮坪沉积。探讨和对比了各类型沉积体系的沉积特征及其之间的差异性。  相似文献   

Re–Os and U–Pb Geochronology of the Erlihe Pb–Zn Deposit, Qinling Orogenic Belt, Central China, and Constraints on Its Deposit Genesis     

ZHANG Fan  LIU Shuwen  LI Qiugen  SUN Yali  WANG Zongqi  YAN Quanren  YAN Zhen 《《地质学报》英文版》2011,85(3):673-682

The Erlihe Pb–Zn deposit is an important mine of the Pb–Zn metallogenic zone in the South Qinling Orogen. It has been considered a sedimentary exhalative deposit in previous investigations because the ore body occurs concordantly at the transitional location of an upright fold. Re and Os isotopic analyses for paragenetic pyrites with sphalerite and galena from the ore body have been used to determine the timing of mineralization and to trace the source of metallogenic materials. The Re–Os isotopic data of four pyrite samples construct an isochron, yielding a weighted average age of 226±17 Ma (mean square weighted deviation=1.7), which is considered the main mineralization age. A dioritic porphyrite vein sample, showing weaker mineralization, was also dated using the SHRIMP zircon U–Pb isotopic method to constrain the youngest metallogenic age of the ore deposit, because it distributes along a group of tensional joints cutting not only the upright fold in the deposit field, but also the main ore bodies. The dioritic porphyrite sample yields a weighted mean 206Pb/238U age of 221±3 Ma, which is slightly younger than the Re–Os isotopic isochron age of the pyrites, considered as the upper age limit of the mineralization, namely the ending age of the mineralization. The Os isotopic compositions of sulfide minerals distribute within a range between Os isotopic compositions of the crust and the mantle, indicating that the ore deposit can be derived from magma-related fluid, and the metallogenic materials are most likely derived from the mixing source of the crust and the mantle. The Erlihe Pb–Zn deposit and associated dioritic porphyrite vein, important records of Qinling tectonic–magmatism–mineralization activities, were formed during the Triassic collisional orogeny processes.  相似文献   

方差技术在生物礁识别中的应用     

屈大鹏  肖秋红  曾臻  彭俊 《物探化探计算技术》2011,33(2):129-133

在海相碳酸盐岩勘探中,生物礁滩的识别对确定储层有利相带具有重要意义.方差技术是检测地下断层、地层不连续变化现象及异常地质体卓有成效的一种技术,这里首先介绍了它的基本原理,然后重点展示和分析该技术在YB生物礁识别,沉积相带刻画中的应用成果,证实其技术优势和良好的应用前景.  相似文献   

U–Pb and Re–Os geochronology and geodynamic setting of the Dabaoshan polymetallic deposit, northern Guangdong Province, South China     

Lei Wang  Mingan Hu  Zhen Yang  Wenjun Qu  Jinlong Xia  Kaixu Chen 《Ore Geology Reviews》2011,43(1):40-49

The Dabaoshan polymetallic deposit in northern Guangdong Province contains iron, copper, lead, zinc, molybdenum, tungsten and sulfur mineral resources. Porphyry-type Mo(W) and skarn-type Mo-W mineralization occurs along the internal and external contact zones of the granodioritic porphyry, respectively. LA-ICP-MS U–Pb dating of zircons from two granodioritic porphyry samples yielded a weighted mean ²⁰⁶Pb/²³⁸U age of 175.8 ± 1.5 Ma (MSWD = 0.037) and 175.0 ± 1.7 Ma (MSWD = 0.41). They can be pooled together to yield a combined weighted age of 175.4 ± 1.6 Ma (MSWD = 0.26), which is interpreted as the emplacement age of the granodioritic porphyry. Re–Os dating of three molybdenite samples from porphyry and skarn ores yielded consistent model ages of 163.2 ± 2.3 Ma to 165.2 ± 2.4 Ma, with a weighted mean of 163.9 ± 1.3 Ma (MSWD = 0.81), which is the age of Mo–W mineralization. These ages are consistent with the molybdenite Re–Os model age (164.7 ± 3 Ma) measured by Mao et al. (2004a) for the stratiform Cu–Pb–Zn orebody, and they can yield a weighted mean of 164.0 ± 2.5 Ma (MSWD = 0.16). This implies that Mo–W and Cu–Pb–Zn mineralization in the Dabaoshan polymetallic deposit are the products of one mineralization event. The mineralization in the deposit coincides closely with that of Mo-polymetallic mineralization (164–149 Ma) elsewhere in the Nanling region, comprising an important polymetallic metallogenic belt of south China, and corresponds to the second episode of Mesozoic metallogenesis in South China. Combined with previous studies, we suggest that the Dabaoshan polymetallic deposit is related to post-collisional lithosphere extension in the Nanling region of South China. Geological data and Pb isotopic evolution diagrams, together with stable isotopic data of fluid inclusions (δ¹⁸O = − 3.75–7.0‰, δD = − 50.7 to − 56.1‰) and ore sulfides (δ³⁴S = − 2–3‰), suggest a genetic relationship between the Dabaoshan polymetallic deposit, the granodioritic porphyry and the dacitic porphyry. These data, combined with the Re content (64.7 to 102.4 ppm) of molybdenite, indicate that the ore-forming components were derived from mixed crustal and mantle sources.  相似文献   

新疆磁海铁矿床中黑柱石的发现及其地质意义     

唐萍芝  王玉往  王京彬  龙灵利  张会琼  廖震 《矿物学报》2011,31(1):9-16

黑柱石是一种不常见的夕卡岩标型矿物,本次研究在新疆磁海矿区首次发现黑柱石。本文对磁海矿区的黑柱石产出地质环境、矿物共生组合、化学成分、光学性质等进行了研究。化学成分均由电子探针分析求得,计算化学简式为Ca0.98(Fe1.72Mn0.07Mg0.11)1.902+(Fe0.95Al0.03)0.983+[Si2.00O7]O(OH)。磁海矿区黑柱石的形成与基性次火山热液活动有关,是一种特殊的退变质(蚀变)夕卡岩矿物;在成矿作用晚期,随着热液活动加强,早期夕卡岩矿物可退变质形成黑柱石。黑柱石形成时间较晚,对早期形成的磁铁矿起贫化作用。将磁海矿区黑柱石与国内外其它矿区黑柱石的化学成分进行了对比,认为磁海矿区黑柱石为普通黑柱石。黑柱石在常用的矿物中较少提及,应该引起重视。  相似文献   

准噶尔盆地石南31井区清水河组油气水层分布规律     

王威  陈维权  宠树伟  韦雨  寇子健  李臻 《新疆地质》2011,29(2):194-197

针对石南31井区储层岩性多变、油气水关系复杂等问题,按不同岩性识别油气层、水层和干层,据油气不同测井响应特征进一步识别油层和气层.将储层划分为细砂岩、中粗砂岩和砂砾岩3类,识别储层流体性质,分析油藏分布特征,指出油层、隔夹层平面分布特征,探讨油气水层分布规律.结果表明,石南31井区主要有4个油藏.储层所含流体有油、水和气,中北部细砂岩储层为纯油层,南部中粗砂岩储层为水层.气层从南到北分布于全区,主要位于油藏北部和东部局部区域,为今后解释工作具很好指导意义.  相似文献   

江西武山花岗闪长斑岩中黑云母成分特征及其成岩成矿意义   总被引：4，自引：0，他引：4  

东前  杜杨松  曹毅  庞振山  宋林旭  郑震 《矿物岩石》2011,31(2)

江西武山花岗闪长斑岩与矽卡岩铜矿在成因上密切相关,通过对其中的黑云母进行的岩相学观察和详细的矿物化学分析来探讨黑云母的形成条件及其成岩成矿意义。电子探针分析结果表明,武山花岗闪长斑岩中的黑云母富镁贫铁低铝高钛,属镁质黑云母。其AlⅥ为0.03~0.19,w(ΣFeO)/w(ΣFeO+MgO)为0.531~0.567,w(MgO)为12.80%~14.06%,指示武山花岗闪长斑岩属壳幔混源的I型花岗岩。黑云母结晶的温度为720℃~750℃,logfO2为-11.6~-12.5,压力为86 MPa~103 MPa,对应的侵位深度为2.84 km~3.39 km,表明该岩体形成于相对高温较浅环境,具有较大成矿潜力,有利于武山铜矿的形成。  相似文献   

东秦岭秋树湾-雁来岭两种不同类型的花岗岩及其构造意义   总被引：3，自引：0，他引：3  

秦臻  戴雪灵  邓湘伟 《矿物岩石》2011,31(3)

秋树湾铜钼矿的成矿母岩—秋树湾花岗斑岩具有高硅、高铝、高Ba、高Sr、富碱、富钾、低镁、贫钙、低稀土总量、铕异常不明显、富集大离子亲石、低Nb和Ti等特点,与苏格兰北部高Ba-Sr花岗岩类似。雁来岭花岗岩较秋树湾花岗岩具全碱指数、铝质指数、ΣREE更高,δEu异常更明显,大离子亲石元素的富集程度差等特点,与低Ba-Sr花岗岩类似。秋树湾高Ba-Sr花岗岩的产出说明该区在晚侏罗—早白垩世发生过壳幔混合作用,代表当时本区可能处于碰撞造山后的局部伸展作用的大地构造环境中。  相似文献   

祁连山老虎沟12号冰川冰内结构特征分析   总被引：2，自引：0，他引：2  

武震  张世强  刘时银  杜文涛 《地球科学进展》2011,26(6):631-641

利用探地雷达(Ground Penetration Radar,GPR)调查冰川冰内结构和冰层厚度是一种监测冰川变化常用手段.应用麦克斯维(Maxwell)方程的二维时域有限差分(FDTD)方法,通过将模拟图像与老虎沟12号冰川的实测图像的对比,分析了雷达剖面中的几种反射特征,如冰裂隙、融洞、暖冰等.对比结果表明,GP...  相似文献   

盐湖卤水锂资源及其开发进展   总被引：7，自引：0，他引：7  

高峰  郑绵平  乜贞  刘建华  宋彭生 《地球学报》2011,32(4):483-492

随着全球资源与环境问题的日益突出,锂资源的开发和利用受到人们的高度关注.由于盐湖卤水中含有丰富的锂资源,所以对其锂资源的开发利用具有重要意义.本文在全球盐湖卤水锂资源的分布及其水化学分类特征论述的基础上,对目前盐湖卤水锂资源的提取工艺进行了比较分类,对卤水锂资源的开发进展情况进行了综述.指出我国盐湖卤水锂资源的开发利用...  相似文献