西沙石岛生物礁的矿物组成及其环境指示意义   总被引：3，自引：0，他引：3       下载免费PDF全文

翟世奎  米立军  沈星  刘新宇  修淳  孙志鹏  曹佳琪 《地球科学》2015,40(4):597-605

通过对西科1井岩心碳酸盐岩样品进行矿物组成分析, 来研究礁体的发育过程和古海洋环境的变化.初步研究结果表明: 西科1井岩心碳酸盐岩的矿物由低镁方解石、高镁方解石、文石和白云石组成.矿物组成特征表明, 井深35.4 m处为一重要的地层界面或环境变化界面.在岩心(井深0~748 m)中共识别出5个白云岩层, 其中上新统莺歌海组一层(井深: 289.3~312.3 m, 厚约23 m), 上中新统黄流组三层(分别位于井深: 373.3~412.7 m, 厚约39.4 m; 424.7~450.6 m, 厚约26.1 m; 469.70~564.96 m, 厚约95.2 m), 中中新统梅山组一层(井深: 615.20~636.96 m, 厚约21.7 m).各层的白云岩化程度不尽相同, 5层白云岩中白云石矿物含量的最大值在79.3%~100%之间.生物礁的发育主要受控于古海洋环境的变化, 与古气候变化有关的海平面升降间接地控制了岛礁碳酸盐岩的白云岩化作用.石岛西科1井中的5层白云岩应该是在较长时间稳定环境条件下发育而成, 主要应该是蒸发泻湖渗透回流作用下早期形成的方解石类碳酸岩白云岩化的结果, 但并不排除混合水白云岩化作用的可能性.   相似文献   

加拿大纽芬兰省稀有稀土矿化特征与勘查进展   总被引：1，自引：0，他引：1  

刘敬党  梁帅  张艳飞  翟富荣 《地质科技情报》2015,(1):167-172

纽芬兰省稀有稀土成矿地质条件优越,矿化主要与侵入的过碱性长英质岩及其喷出岩有关,矿化围岩为中元古代火成岩系,矿床成因类型为岩浆型和热液交代型,且以前者为主,典型矿床为世界级大型原生Strange Lake(Nd-Y-Zr-REE)矿床。目前,地球化学方法是区内寻找稀有稀土矿床最有效的勘探工具,拉布拉多主要勘查区为Letitia Lake、Red Wine Mountains、Flowers River和Strange Lake,纽芬兰岛主要勘查区为Fortune Bay、Clode Sound、Trinity Bay和Lost Pond。  相似文献   

Impact of the geological structure on pulsating hydraulic fracturing     

Ni Guanhua  Lin Baiquan  Zhai Cheng 《Arabian Journal of Geosciences》2015,8(12):10381-10388

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Eutectic metal + troilite + Fe‐Mn‐Na phosphate + Al‐free chromite assemblage in shock‐produced chondritic melt of the Yanzhuang chondrite     

Xiande Xie  Ming Chen  Shuangmeng Zhai  Fuya Wang 《Meteoritics & planetary science》2014,49(12):2290-2304

An assemblage with FeNi metal, troilite, Fe‐Mn‐Na phosphate, and Al‐free chromite was identified in the metal‐troilite eutectic nodules in the shock‐produced chondritic melt of the Yanzhuang H6 meteorite. Electron microprobe and Raman spectroscopic analyses show that a few phosphate globules have the composition of Na‐bearing graftonite (Fe_,Mn,Na)₃(PO₄)₂, whereas most others correspond to Mn‐bearing galileiite Na(Fe,Mn)₄(PO₄)₃ and a possible new phosphate phase of Na₂(Fe,Mn)₁₇(PO₄)₁₂ composition. The Yanzhuang meteorite was shocked to a peak pressure of 50 GPa and a peak temperature of approximately 2000 °C. All minerals were melted after pressure release to form a chondritic melt due to very high postshock heat that brought the chondrite material above its liquidus. The volatile elements P and Na released from whitlockite and plagioclase along with elements Cr and Mn released from chromite are concentrated into the shock‐produced Fe‐Ni‐S‐O melt at high temperatures. During cooling, microcrystalline olivine and pyroxene first crystallized from the chondritic melt, metal‐troilite eutectic intergrowths, and silicate melt glass finally solidified at about 950–1000 °C. On the other hand, P, Mn, and Na in the Fe‐Ni‐S‐O melt combined with Fe and crystallized as Fe‐Mn‐Na phosphates within troilite, while Cr combined with Fe and crystallized as Al‐free chromite also within troilite.  相似文献   

Reply to Comment by M. Chaussidon and F. Robert: Are the boron isotopic ratio and abundance homogeneous or heterogeneous in meteorites?     

Mingzhe Zhai 《Meteoritics & planetary science》1997,32(2):324-326

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相接双星SW Lac的视向速度观测及其活动性的研究     

翟迪生  陆文贤 《中国天文和天体物理学报》1989,(3)

本文发表了WUMa型相接双星SW Lac的1984年视向速度观测,它给出的新的分光质比q_(sp)=m_2/m_1=1.255±0.011。通过光变曲线观测和视向速度曲线观测的联合分析,得出改进了的双星绝对参量:M_1=0.78M_⊙,M_2=0.96M_⊙,R=0.91R_⊙和R_2=1.00R_⊙,在此基础上,对SW Lac双星的周期变化,可能的质量交流和损失,以及黑子活动等作了详细分析讨论。  相似文献   

Variation of stress during the rupture process of the 1995 <Emphasis Type="Italic">M</Emphasis><Subscript>L</Subscript>=4.1 Shacheng,Hebei, China,earthquake sequence     

Chen Xue-zhong  Xu Xiang-tong  Zhai Wen-jie 《地震科学（英文版）》2005,18(3):297-302

According to the rupture dynamics of earthquakes, variations of the apparent stress and the difference between the static stress drop and the dynamic stress drop during the rupture of earthquakes are analyzed for the July 20, 1995 M _L=4.1 Shacheng, Hebei, China, earthquake sequence. Results obtained show that the apparent stress for main-shock is about 5 MPa, and the average apparent stress for aftershocks 0.047 MPa. During the rupture of the main-shock, the dynamic stress drop is approximately 1.6 times greater than the static stress drop with the difference of nearly 2.7 MPa. The dynamic stress drop is less than the static stress drop for all aftershocks with the average difference of ?0.75 MPa. Therefore, when the mainshock occurs the final stress on the focal fault is higher than the dynamic frictional stress, corresponding to that the fault is abruptly locked. When the aftershocks occur the final stress on the focal fault is lower than the dynamic frictional stress, corresponding to that the fault overshoots. It can be seen from the above results that there could be some differences in the physic processes between the mainshock and the aftershocks.  相似文献   

Discovery of double-peaking potassic volcanic rocks in Langshan Group of the Tanyaokou hydrothermal-sedimentary deposit,Inner Mongolia,and its indicating significance   总被引：2，自引：0，他引：2  

PENG Runmin  ZHAI Yusheng  WANG Zhigang & HAN Xuefeng . Key Laboratory of Lithospheric Tectonics  Lithoprobing Technology  Ministry of Education  China University of Geosciences  Beijing  China  . Inner Mongolia Geological Prospecting Institute  Ministry of Chemical Industry  Hohhot  China Correspondences should be addressed to Peng Runmin 《中国科学D辑(英文版)》2005,48(6):822-833

Since the mid-1980s,Tanyaokou large Zn-Cu-Fe sulfides deposit,located at the southwest end of Langshan-Zhaertaishan-Bayan Obo Mesoproterozoic metallogenic belt in the west section of the northern margin of the North China Platform[1?9](Fig.1),has been confirmed to be submarine volcanic exhalative-sedimentary metamorphosed deposit hosted in the miogeosynclinal mud-carbonaceous formation of the Langshan Group(LG)[1],or submarine volcanic exha-lative-deposition-altered deposit[2]or stratabo…  相似文献   

Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence   总被引：7，自引：0，他引：7  

FAN Qicheng    ZHANG Hongfu  SUI Jianli  ZHAI Mingguo  SUN Qian & LI Ni . Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China  . Institute of Geology  China Seismological Bureau  Beijing  China 《中国科学D辑(英文版)》2005,48(8):1089-1105

Studies on the deep-seated xenoliths from global volcanoes reveal that the present petrological crust-mantle boundary between the lower crust and the upper mantle actually is a transitional layer from mainly mafic granulites to ultramafic spinel lher-zolites[1,2], i.e. a transitional zone distinctive from the seismological Moho[3]. Oceanic lithosphere crust- mantle transitional zone can be established from the study on the exposed ophiolites. However, as for the continental lithosphere, since …  相似文献   

Fluid evolution in the Rushan lode gold deposit of Jiaodong Peninsula, eastern China   总被引：2，自引：0，他引：2  

Fang-Fang Hu  Hong-Rui Fan  Ming-Guo Zhai  Cheng-Wei Jin 《Journal of Geochemical Exploration》2006,89(1-3):161

The Rushan gold deposit in the Jiaodong Peninsula is currently the largest lode gold in China. Gold occurs mainly in pyrite- and polymetallic sulfide–quartz vein/veinlet stockworks. Fluid inclusions in the deposit are divided into three main types, namely CO₂–H₂O, H₂O–CO₂ ± CH₄ and aqueous ones. Microthermometric data show that the pre-gold fluids were CO₂-dominant (X_CO2 up to 0.53), and the total homogenization temperatures fall in the range of 298377 °C. These fluids, modified by fluid/wallrock reactions, gradually evolved into fluids with less CO₂ (X_CO2 = 0.010.19) in the main ore-forming stage, and the total homogenization temperatures range from 170 to 324 °C. Hydrogen and oxygen stable isotope data suggest that ore-forming fluids were mixture of magmatic and meteoritic origin. Co-occurrence of gold and sulfides implies that gold was most likely transported in the form of gold–sulfide complexes. The wide distribution of CO₂ inclusions means that the pH variation during gold transportation was controlled by CO₂ buffering.  相似文献