蒙古戈壁阿尔泰巴音陶勒盖地区二长花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义   总被引：1，自引：1，他引：0  

付超  李俊建  唐文龙  党智财  Orolmaa Demberel 《地质通报》2016,35(4):565-571

蒙古戈壁阿尔泰省巴音陶勒盖地区地处南戈壁-阿尔泰构造带南缘,区内构造活动活跃,中酸性侵入岩比较发育。采用LA-ICP-MS锆石U-Pb测年技术,对区内二长花岗岩中的锆石进行同位素年龄研究。阴极发光图像显示,锆石颗粒多为自形-半自形,且有明显的初始岩浆振荡环带,少见蚀变微区,结合较高的Th/U值(0.65~1.79),断定其为典型的岩浆成因锆石;30颗锆石的~(206)Pb/~(238)U年龄加权平均值为300.2±0.9Ma,显示二长花岗岩成岩时代为晚石炭世,代表了华力西中期的一次构造-岩浆事件,为约束南戈壁-阿尔泰构造带晚石炭世深成岩浆活动时限提供了新证据。  相似文献   

蒙古科布多省阿拉腾索音博地区辉长岩LA-ICP-MS锆石U-Pb年龄及其地质意义     

付超  李俊建  唐文龙  党智财  Orolmaa Demberel 《地质通报》2016,35(4):572-577

蒙古科布多省阿拉腾索音博地区地处阿尔泰构造带南缘,由一系列弧盆系及增生杂岩带组成。区内发育一条近东西向辉长岩带,辉长岩15颗锆石分为2类:一类具明显条带韵律环带,一类内部均匀干净,二者均不具核边结构,不含包体,结合高Th/U值(0.46~0.68),确定为典型的基性岩浆锆石;锆石LA-ICP-MS年龄加权平均值为317.6±1.6Ma,厘定其成岩时代为晚石炭世。研究对比表明,该辉长岩带形成于板块俯冲碰撞的尾声阶段,是阿尔泰造山运动大背景下区域基性岩浆活动的产物。  相似文献   

Determining sources of mine water based on hydraulic characteristics analysis of a fault system     

Mei Yao  Peigui Liu  Manting Shang  Yuezan Tao  Chao Lei  Lugan Cao 《Environmental Earth Sciences》2016,75(10):858

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Statistical meso-damage model for quasi-brittle rocks to account for damage tolerance principle     

Heng Zhao  Chao Zhang  Wen-gui Cao  Ming-hua Zhao 《Environmental Earth Sciences》2016,75(10):862

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Pattern analysis of simple transverse dunes in China’s Qaidam Basin,north of the Kunlun Mountains   总被引：2，自引：0，他引：2  

Chao Li  Zhibao Dong  Xujia Cui  Feng Bao 《Environmental Earth Sciences》2016,75(9):729

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Geochemistry of geothermal waters from the Gonghe region,Northwestern China: implications for identification of the heat source     

Mingliang Liu  Qinghai Guo  Xiaobo Zhang  Jin Luo  Jiexiang Li  Chao Zhou  Wei Guo  Canhai Zhang  Mingcheng Zhu 《Environmental Earth Sciences》2016,75(8):682

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Mineralization time and tectonic setting of the Zhengguang Au deposit in the Duobaoshan ore field,Heilongjiang Province,NE China     

Yu-Jie Hao  Yun-Sheng Ren  Ming-Xin Duan  Xuan Zhao  Qun Yang  Kuang-Yin Tong  Chao Li 《Arabian Journal of Geosciences》2016,9(15):655

The Zhengguang deposit, a representative large gold deposit in the Duobaoshan ore field in NE China, is located in the northeast of the Central Asian Orogenic Belt (CAOB). Ore body emplacement was structurally controlled and occurs mainly at the contact zone between the strata of Duobaoshan Formation and an Ordovician diorite stock. The diorite rocks have a close genetic relationship with Au mineralization. Re–Os isotope dating of Au-bearing pyrite yields an isochron age of 506 ± 44 Ma (MSWD = 15). Based on present and previous dating results, it can be concluded that the Zhengguang deposit formed at ~480 Ma. The mineralization time of the Zhengguang deposit is nearly identical to those of the Duobaoshan and Tongshan deposits, indicating they are all derived from the same metallogenic system. The Duobaoshan-style porphyry Cu–Mo mineralization may exist at deeper levels at Zhengguang. The geochemical characteristics of the Zhengguang dioritic rocks presented in this paper are similar to those of bajaitic high-Mg andesite, and the magmas originated from a mantle wedge metasomatized by melts from a subducting oceanic slab at an active continental margin setting. The Ordovician magmatic–metallogenic events in the Duobaoshan ore field were caused by the westward subduction of an oceanic slab located between the Xing’an and Songliao blocks. It is worth pointing out that the Zhengguang deposit is the oldest known Phanerozoic Au deposit in NE China. Further studies of this deposit will improve understanding of the regularity of ore formation and aid mineralization forecast across the Duobaoshan region.  相似文献   

不同刚度植物杆群对规则波传播及紊动特性影响研究     

谭超  黄本胜  刘达  邱静  王珍  吉红香 《海洋工程》2016,34(6):38-45

以不同刚度硅胶圆杆群为概化植物模型,测定其抗弯弹性模量,通过波浪水槽实验,研究规则波在不同刚度植物杆群内的流速分布、紊动特征及不同刚度杆群的消浪效果。实验结果表明,当波浪通过柔性杆群时,受其摆动的影响,流速周期变化从单峰型逐渐转变成双峰型,杆群刚度越小形成的二次波峰越明显;不同刚度杆群内水体紊动强度变化显示,杆群刚度越大,造成杆群内水体的紊动强度越大;随着杆群抗弯弹性模量的增大,其消浪系数也增大,消浪系数的增长与材料的抗弯弹性模量值非线性关系,而是在某一弹性模量范围内,对消浪系数的影响较为敏感。  相似文献   

Development of A Depth-Integrated Longshore Current Model with Unstructured Grids     

陈超  张庆河 《海洋工程》2016,(5):718-732

A depth-integrated model for simulating wave-induced longshore current was developed with unstructured grids. Effects of surface roller and horizontal mixing under combined waves and currents were incorporated in the numerical model. Recommended values of model coefficients were also proposed based on sensitivity analysis. Field observations and three series of laboratory measurements including two cases conducted on the plane beach and one implemented on the ideal inlet were employed to examine the predictive capability of this model. For the field case and laboratory cases conducted on the plane beach, numerical results were compared favorably with the measured data. For the case with an ideal inlet, simulated circulation pattern is supposed to be reasonable although some deviations between numerical results and measured data still can be detected.  相似文献   

Application of Linear Mean-Square Estimation in Ocean Engineering     

王莉萍  陈柏宇  陈超  陈正寿  刘桂林 《海洋工程》2016,(1):149-160

The attempt to obtain long-term observed data around some sea areas we concern is usually very hard or even impossible in practical offshore and ocean engineering situations. In this paper, by means of linear mean-square estimation method, a new way to extend short-term data to long-term ones is developed. The long-term data about concerning sea areas can be constructed via a series of long-term data obtained from neighbor oceanographic stations, through relevance analysis of different data series. It is effective to cover the insufficiency of time series prediction method’s overdependence upon the length of data series, as well as the limitation of variable numbers adopted in multiple linear regression model. The storm surge data collected from three oceanographic stations located in Shandong Peninsula are taken as examples to analyze the number-selection effect of reference oceanographic stations (adjacent to the concerning sea area) and the correlation coefficients between sea sites which are selected for reference and for engineering projects construction respectively. By comparing the N-year return-period values which are calculated from observed raw data and processed data which are extended from finite data series by means of the linear mean-square estimation method, one can draw a conclusion that this method can give considerably good estimation in practical ocean engineering, in spite of different extreme value distributions about raw and processed data.  相似文献