内蒙古白乃庙金矿断裂构造控矿研究   总被引：5，自引：1，他引：5       下载免费PDF全文

和钟铧  周立宏等 《地质与勘探》2001,37(2):28-31

白乃庙金矿由石英脉型和蚀变岩型金矿组成，并受断裂及其破碎带控制，研究了白乃庙金矿断裂构造与成矿关系，断裂构造趋势面与找矿及矿体在断裂中的富集规律，并对成矿远景进行了预测。  相似文献   

新疆北部阿尔泰地区库尔提蛇绿岩：古弧后盆地系统的产物   总被引：40，自引：3，他引：40       下载免费PDF全文

许继峰  陈繁荣  于学元  牛贺才  郑作平 《岩石矿物学杂志》2001,20(3):344-352

位于新疆北部富蕴县库尔提一带的晚古生代变质玄武岩和辉长岩系含有似岛弧火山岩（arc-like)和似洋中脊玄武岩（MORB－like)成分的两种组分，岩石以出现不同程度的LREE亏损和Nb、Ta等元素的负异常为特征，在成分上非常相似于现代弧后盆地（Mariana和Okinawa弧后盆地）的玄武岩。我们厘定这套变质的镁铁质火成岩为弧后盆地蛇绿岩，它们很可能代表了晚古生代古亚洲洋北侧的一个洋内岛弧的弧后盆地系统，表明晚古生代早期新疆北部地区处于与古亚洲洋俯冲有关的岛弧环境，该古洋在晚石炭世－二叠纪消减消失后，两侧西伯利亚和哈萨克－准噶尔板块才开始碰撞和造山。  相似文献   

海南岛前寒纪岩石圈演化的记录：基性岩类岩石地球化学证据   总被引：8，自引：1，他引：8  

许德如  林舸等 《岩石学报》2001,17(4):598-608

海南岛前寒武纪基性岩类具有的不同的岩石地球化学特征，记录了海南岛前寒武纪大地构造环境和岩石圈的演化史。古中元古代时，琼中屯昌变基性－超基性岩，为大洋型火山岛弧低钾拉斑玄武岩，明显具有镁铁质－玄武质科马提岩特征，来源于高度亏损的地幔；与之同时代的琼西，则为一套具洋底玄武岩和岛弧拉弦玄武岩的过渡型玄武岩，是古俯冲带上部地幔楔和自消减带卷入地幔楔地壳物质所组成的混合端元部分熔融产物，具低亏损地幔特征，产生于弧后（或弧间）盆地环境；中新元古代的琼西变基性－超基性岩具铁镁质－超铁镁质科马提岩特征，来源于较高亏损的地幔，产于大洋板块边缘的构造环境。据此，可以推测，海南岛前寒武纪岩石圈演化至少经历了古中元古代的古板块俯冲、中新元古代的裂解二次事件，并伴随洋盆的出现。  相似文献   

Geochemistry and magnetostratigraphy of deccan flows at Anjar, Kutch     

A. D. Shukla  N. Bhandari  Sheela Kusumgar  P. N. Shukla  Z. G. Ghevariya  K. Gopalan  V. Balaram 《Journal of Earth System Science》2001,110(2):111-132

Chemical analysis of nine Deccan flow basalts at Anjar, Kutch, western India, indicates that all, except the uppermost flow F-9, are alkaline. In their major and trace element composition, the alkali basalts resemble Ocean island basalts (OIB). Similarities of many diagnostic trace element ratios (e.g. Sm/Nd, Ba/Nb,Y/Nb and Zr/Nb) are similar to those found in the Réunion Island basalts. The uppermost basalt is tholeiitic and chemically resembles the least contaminated Deccan basalt (Ambenali type). The Anjar basalts have iridium concentration ranging between 2 and 178 pg/g. Some of these values are higher by about an order of magnitude compared to the Ir concentration in other basalts of the Deccan. A synthesis of chemical, palaeomagnetic and geochronologic data enables us to construct a chemical and magnetic stratigraphy for these flows. The three flows below the iridium enriched intertrappean bed (IT III) show normal magnetic polarity whereas all except one of the upper basalts show reversed magnetic polarity. The sequence seems to have started in polarity zones 31N and probably continued up to 28R or 27R. The results presented here support the view that Deccan volcanism in Kutch occurred on a time span of a few million years.  相似文献   

Petrochemical Investigation of the Antique Ophiolite (Philippines): Implications on Volcanogenic Massive Sulfide and Podiform Chromitite Deposits   总被引：5，自引：0，他引：5  

Rodolfo A. TAMAYO Jr    Graciano P. YUMUL Jr    René C. MAURY  Mireille POLVÉ  Joseph COTTEN  Marcel BOHN 《Resource Geology》2001,51(2):145-164

Abstract: The Antique ophiolite, located in Panay island (west‐central Philippines), corresponds to several tectonic slices within the suture zone between the Philippine Mobile Belt (PMB) and the North Palawan Block (NPB). It includes dismembered fragments of a basaltic sequence, dominantly pillow‐lavas with minor sheet flows, rare exposures of sheeted dikes, isotropic gabbros, subordinate layered mafic and ultramafic rock sequences and serpentinites. Most of the ophiolite units commonly occur as clasts and blocks within the serpentinites, which intrude the whole ophiolitic body, as well as, the basal conglomerate of the overlying Middle Miocene sedimentary formation. The volcanic rock sequence is characterized by chemical compositions ranging from transitional (T)‐MORB, normal (N)‐MORB and to chemistry intermediate between those of MORB and island arc basalt (IAB). The residual upper mantle sequence is harzburgitic and generally more depleted than the upper mantle underlying modern mid‐oceanic ridges. Calculations using whole‐rock and mineral compositions show that they can represent the residue of a fertile mantle source, which have undergone degrees of partial melting ranging from 9‐22.5 %. Some of the mantle samples display chondrite‐nor‐malized REE and extended multi‐element patterns suggesting enrichments in LREE, Rb, Sr and Zr, which are comparable to those found in fore‐arc peridotites from the Izu‐Bonin‐Mariana (IBM) arc system. The Antique ultramafic rocks also record relatively oxidizing mantle conditions (Δlog f_O2 (FMQ)=0.9‐3.5). As a whole, the ophiolite probably represents an agglomeration of oceanic ridge and fore‐arc crust fragments, which were juxtaposed during the Miocene collision of the PMB and the NPB. The intrusion of the serpentinites might be either coeval or subsequent to the accretion of the oceanic crust onto the fore‐arc. Volcanogenic massive sulfide (VMS) deposits occur either in or near the contact between the pillow basalts and the overlying sediments or interbedded with the sediments. The morphology of the deposits, type of metals, ore texture and the nature of the host rocks suggest that the formation of the VMS bodies was similar to the accumulation of metals around and in the subsurface of hydrothermal vents observed in modern mid‐oceanic ridge and back‐arc basin rift settings. The podiform chromitites occur as pods and subordinate layers within totally serpentinized dunite in the residual upper mantle sequence. No large coherent chromitite deposit was found since the host dunitic rocks often occur as blocks within the serpentinites. It is difficult to evaluate the original geodynamic setting of the mineralized bodies since the chemistry of the host rocks were considerably modified by alteration during their tectonic emplacement. A preliminary conclusion for Antique is that the VMS is apparently associated with a primitive tholeiitic intermediate MORB‐IAB volcanic suite, the chemistry of which is close to the calculated composition of the liquid that coexisted with the podiform chromitites.  相似文献   

Oxygen and Carbon Isotope Study of Calcite and Dolomite in the Disseminated Au-Ag Telluride Bulawan Deposit, Negros Island, Philippines     

Victor B. MAGLAMBAYAN  Daizo ISHIYAMA  Toshio MIZUTA  Osamu MATSUBAYA  Yohei ISHIKAWA 《Resource Geology》2001,51(2):107-116

Abstract: The disseminated Au‐Ag telluride Bulawan deposit, Negros island, Philippines, is hosted by dacite porphyry breccia pipes which formed in a Middle Miocene dacite porphyry stock. Electrum and Au‐Ag tellurides occur mostly as grains intergrown with or filling voids between sphalerite, pyrite, chalcopyrite, galena and tennantite. Calcite, quartz and rare dolomite are the principal gangue minerals. Four types of alteration were recognized in the deposit, namely; propylitic, K‐feldspar‐sericitic, sericitic and carbonate alteration. Carbonate alteration is correlatable to the gold deposition stage and occurs mostly along fault zones. The δ¹⁸O and δ¹³C compositions of calcite and dolomite in propylite zone and ore‐stage dacite porphyry breccia were determined. The δ¹⁸O values of calcite in propylitized andesite range from +12.2 to +14.7%, and their δ¹³C values range from ‐6.1 to ‐1.0%. The δ¹⁸O values of calcite and dolomite in sericite‐ and carbonate‐altered, mineralized dacite porphyry breccia and dacite porphyry rocks range from +15.1 to +23.1%, and the δ¹³C values of calcite and dolomite range from ‐3.9 to +0.9%. The δ¹⁸O and δ¹³C values of the hydrothermal fluids were estimated from inferred temperatures of formation on the basis of fluid inclusion microthermometry. The δ¹⁸O values of hydrothermal fluid for the propylitic alteration were calculated to be +8.5 ‐ +9.5%, assuming 375°C. On the other hand, the δ¹⁸O values of ore solutions for base metal and Au mineralization were computed to be +13.6 ‐ +14.6%, assuming 270°C. The hydrothermal fluids that formed the Bulawan deposit are dilute and ¹⁸O‐enriched fluids which reacted with ¹⁸O‐ and ¹³C‐rich wallrocks such as limestone.  相似文献   

SOME NEW UNDERSTANDINGS OF LAND-SURFACE PROCESSES IN ARID AREA FROM THE HEIFE     

胡隐樵  高由禧 《Acta Meteorologica Sinica》1996,(2)

The survey for the HEIFE(Atmosphere-Land Surface Processes Experiment at Heihe RiverBasin,Western China)is given in the paper.The following basic subjects for land-surface process-es in arid areas are studied:(1)the general characteristics of the energy budget on ground surfacein arid areas;(2)the parameterization of the land surface processes;(3)the interaction betweenoasis and its desert circumstances,a special phenomenon in arid areas.The analysis shows that thesensible heat flux in the surface energy budget is in the majority,and the latent heat flux may beneglected.The influence of atmospheric stratification stability on the turbulent transfer of energyand substance must be considered in parameterization of land surface processes in arid areas.The“cold island effect”phenomenon in oasis and the“humidity inversion”phenomenon in desert nearoasis are the result of the interaction between them.The results would improve the understandingof land surface processes in arid areas.  相似文献   

Collision orogeny at arc-arc junctions in the Japanese Islands   总被引：1，自引：0，他引：1  

Gaku  Kimura 《Island Arc》1996,5(3):262-275

Abstract In the Japanese Islands, collision tectonics are operating at arc-arc junctions in three regions: Hokkaido, Central Japan and Kyushu. Hokkaido is situated at the junction of the Kuril and Northeast Japan Arcs. The Kuril fore arc sliver collides with the Northeast Japan Arc, and the lower crust of the Kuril Arc thrusts upon the fore arc of the Northeast Japan Arc in Hokkaido. Outcrops of the lower crust are observed in the Hidaka Mountains in the fore arc of the junction area. Central Japan is in the juncture area among the Northeast Japan, Izu-Bonin, and Southwest Japan Arcs. The Izu-Bonin arc is colliding against the Honshu mainland, which has been bent by the collision. Kyushu is a juvenile collision area between the Southwest Japan and Ryukyu Arcs. The fore arc of the Southwest Japan Arc is starting to underthrust beneath the Kyushu islands along the Bungo Strait, where shallow seismicity within the crust is active in terms of the collision. Collision tectonics are observed at most of the arc-arc junctions in the circum-Pacific orogenic belts and may be an important process contributing to the relatively rapid growth of new continental crust in subduction zones.  相似文献   

新疆东天山泥盆纪火山岩岩石学特征及其形成的大地构造环境   总被引：1，自引：0，他引：1  

肖渊甫  茅燕石 《矿物岩石》1992,12(2):34-42

新疆东天山地区泥盆纪火山活动频繁,火山岩广泛发育。火山岩系由钙碱系列(占75％)石英安山岩、英安岩、玄武岩、碱长流纹岩以及大量的火山碎屑岩,和拉斑玄武系列(约占25％)的石英拉斑玄武岩,少量橄榄拉斑玄武岩组成。岩石普遍富含Na_2O,SiO_2,而贫MgO,K_2O,以CaO,属钠质型和普通型。稀有元素配分型式具“三隆起”特征,过渡族元素呈明显的“W”形态,稀土元素为铕平坦或略具亏损的轻稀土富集型。据研究,火山岩由南至北具明显的钾元素地球化学极性。反映其板块构造环境为一俯冲带倾向北的陆壳型岛弧。  相似文献   

对岛状融区房建冻害的几点认识——以沱沱河兵站楼房为例     

黄以职  郭东信 《冰川冻土》1992,(1)

座落在岛状融区中的青藏高原沱沱河兵站楼房,由于跨年度施工,楼房各部位季节冻深和融化速度不一,引起不均匀下沉,致使墙体产生严重裂缝。岛状融区是工程地质环境敏感区。在太阳辐射强烈的青藏高原,现行建筑规范中房屋采暖对冻深的影响系数偏小,建议对北外墙中段和角端应比规范规定系数分别增大0.2和0.3。  相似文献