Late Carboniferous – Middle Permian arc/forearc‐related basin in Central Asian Orogenic Belt: Insights from the petrology and geochemistry of the Shuangjing Schist in Inner Mongolia,China     

YILONG LI  HANWEN ZHOU  FRAUKJE M. BROUWER  WENJIAO XIAO  ZENGQIU ZHONG  JAN R. WIJBRANS 《Island Arc》2011,20(4):535-549

The Solonker Suture Zone is thought to record the terminal evolution of the Central Asian Orogenic Belt (CAOB) in Inner Mongolia. However, two contrasting interpretations of the timing of suturing of the Solonker Suture Zone exist: (i) Permian to Early Triassic; and (ii) Middle Devonian or Late Devonian to Carboniferous. The Shuangjing Schist is exposed in the Linxi area along the Xar Moron Fault Zone, which marks the southern boundary of the Solonker Suture Zone in the eastern section of the CAOB, and thus provides insight into the timing of suturing of the Solonker Suture Zone. Detailed and systematic analysis of the petrology and geochemistry of the Shuangjing Schist shows that the Shuangjing Schist developed by greenschist facies prograde metamorphism of a volcanisedimentary rock series protolith. The volcanic parts of the Shuangjing Schist are a calc‐alkaline series with large volumes of intermediate members and subordinate acidic members. Volcanism occurred in a magmatic arc on the continental margin and was induced by subduction‐related magmatism resulting from mantle metasomatism. The sedimentary parts of the Shuangjing Schist reflect a transition from continental shelf to abyssal plain sedimentation. The formation of the Shuangjing Schist is suggested to be related to closure of an arc/forearc‐related ocean basin. The timing is constrained by a laser ablation inductively coupled plasma–mass spectrometry (LA‐ICP–MS) U–Pb magmatic zircon age of 298 ± 2 Ma from a carbonaceous biotite–plagioclase schist that was intruded by granite at 272 ± 2 Ma. In the Linxi area, southward subduction of the arc/forearc basin led to uplift, thickening, collapse, and erosion of the overriding continental crust. Collapse induced extension and widespread magmatism along the volcanic arc at the northern margin of the North China Craton. The closure of the arc/forearc‐related oceanic basin led to the formation of Late Permian to Middle Triassic collisional granites and the subsequent end of the collision of the Solonker Suture Zone.  相似文献   

Comparison of rhyolites from continental rift,continental arc and oceanic island arc: Implication for the mechanism of silicic magma generation     

Dereje Ayalew  Akira Ishiwatari 《Island Arc》2011,20(1):78-93

We discuss the chemical compositions of rhyolites from three distinct tectonic settings: (i) the continental rift from Ethiopia (both Oligocene–Miocene and Quaternary rhyolites); (ii) the early Miocene continental arc of Japan (the Mt Wasso rhyolites related to the rifting of the Japan Sea); and (iii) the oceanic Izu–Bonin Island Arc. The comparison reveals that the oceanic island arc rhyolites have high contents of CaO, Al₂O₃, and Sr, and extremely low abundance of trace elements including K₂O. In contrast, the Ethiopian continental rift rhyolites are characterized by low contents of CaO, Al₂O₃, and Sr, and high contents of K₂O, and are enriched in the whole range of trace elements. The continental arc Mt Wasso rhyolites are apparently low in Nb content, although they display similar chemical trends to those of the Ethiopian rhyolites. This obvious difference in the chemical signatures of the rhyolites from the three tectonic settings is the consequence of their derivation from different sources. The implication of this result is that fractional crystallization processes were dominant in the rift‐related rhyolites both from continental rift and continental arc regardless of the prevailing tectonic setting and the nature of the crust (age, thickness, composition), whereas the oceanic island arc rhyolites may form through partial melting of young, mafic crust.  相似文献   

SHRIMP dating of magmatism in the Hitachi metamorphic terrane,Abukuma Belt,Japan: Evidence for a Cambrian volcanic arc     

MICHIO TAGIRI  DANIEL J. DUNKLEY  TATSURO ADACHI  YOSHIKUNI HIROI  C. MARK FANNING 《Island Arc》2011,20(2):259-279

Ion microprobe dating of zircon from meta‐igneous samples of the Hitachi metamorphic terrane of eastern Japan yields Cambrian magmatic ages. Tuffaceous schist from the Nishidohira Formation contains ca 510 Ma zircon, overlapping in age with hornblende gneiss from the Tamadare Formation (ca 507 Ma), and meta‐andesite (ca 507 Ma) and metaporphyry (ca 505 Ma) from the Akazawa Formation. The latter is unconformably overlain by the Carboniferous Daioin Formation, in which a granite boulder from metaconglomerate yields a magmatic age of ca 500 Ma. This date overlaps a previous estimate for granite that intrudes the Akazawa Formation. Intrusive, volcanic, and volcaniclastic lithologies are products of a Cambrian volcanic arc associated with a continental shelf, as demonstrated by the presence of arkose and conglomerate in the lowermost Nishidohira Formation. Granitic magmatism of Cambrian age is unknown elsewhere in Japan, except for a single locality in far western Japan with a similar geological context. Such magmatism is also unknown on the adjacent Asian continental margin, with the exception of the Khanka block in far northeastern China. A ‘great hiatus’ in the Paleozoic stratigraphy of the Sino–Korean block also exists in the Hitachi terrane between Cambrian volcanic arc rocks and Early Carboniferous conglomerate, and may indicate a common paleogeographic provenance.  相似文献   

利用灰集进行空间区域拓扑关系不确定性定量分析     

包磊  罗兵  秦小麟 《武汉大学学报(信息科学版)》2011,(6):731-733

针对不确定性空间区域对象间拓扑关系不确定性的定量分析问题,提出了一种具有双隶属度函数的灰集表示模型,利用双隶属度函数的截集将不确定性空间区域对象转化为确定性区域对,借用相关的不确定性空间拓扑关系定性分析模型,将不确定性空间对象间拓扑关系的不确定性量化为一个可信度区间。  相似文献   

边坡滚石运动轨迹分段循环算法   总被引：1，自引：0，他引：1  

俸锦福  张俊红  朱彬  陈宇龙 《中国地质灾害与防治学报》2011,22(4):96-101

边坡滚石是在基本建设中常遇到的一种工程灾害。其防护结构的设计依据主要是边坡滚石的运动轨迹,因而要对这种灾害进行防治,首先要确定滚石的运动轨迹。根据落石运动全过程的三个阶段,即滚动(滑动)运动阶段、抛物运动阶段和与坡面碰撞阶段,利用分段循环算法分别得到了三个运动阶段的运动速度计算公式。以某岩质边坡构建相似模型,将该理论公式应用于落石运动轨迹预测,验证了公式的可行性和有效性。与现有方法相比,分段循环算法具有计算原理简单明确、易于使用等优点。该方法可用于斜坡区滚石运动特征的预测,并可作为斜坡区滚石灾害防治的依据。  相似文献   

塔里木盆地东北缘早古生代构造格局及演化   总被引：3，自引：1，他引：2       下载免费PDF全文

左国朝  李绍雄 《中国地质》2011,38(4):945-960

塔里木盆地东北缘构造带包括了新疆东天山及甘肃—内蒙北山广大地区。本区早古生代塔里木板块与哈萨克斯坦板块的对接带展布于由西段阿其克库都克断裂带向东与石板井—小黄山蛇绿混杂岩一线。晋宁运动(800 Ma)本区经历了广泛的岩浆热事件,西伯利亚板块、哈萨克斯坦板块与塔里木板块曾一度合并到罗迪尼亚超大陆之上。南华—震旦纪古大陆解体,哈萨克斯坦板块及塔里木板块块断区以多岛群体弥散于古亚洲洋内。塔里木板块东段的陆缘区,震旦—寒武纪显示海湾型沉积区。奥陶纪沿花牛山—五峰山—帐房山一线裂解为裂谷带,晚奥陶世末前碰撞期岩浆活动导致裂谷关闭。早、中志留世,古亚洲洋洋壳板片沿着尾亚南—芨芨台子山—白云山—月牙山—洗肠井一线向南俯冲,构筑了公婆泉火山岛弧带及相匹配的红柳河—牛圈子—碱泉子弧后盆地。晚志留世的碰撞初期花岗岩浆运动极为活跃。泥盆纪进入主碰撞期,造山阶段的岩浆热事件波及到隆升中的造山带,在其南缘沉陷为火山-磨拉石前陆盆地。  相似文献   

拓扑多边形自相交判断及纠正方法     

周兰兰  康建荣 《测绘与空间地理信息》2014,(10):33-35

提出了一种解决地形图处理中拓扑多边形自相交问题的方法。首先在原多边形内部构建新多边形,通过判定新多边形的顶点是否为原多边形内点实现了多边形自相交的判断。最后利用三种方式对存在自相交的多边形进行纠正。基于VC＋＋6.0实现相关功能,并以实例验证了这一方法的稳定性和可行性。  相似文献   

关于区间值直观模糊集上的拓扑空间     

曾德胜  吴泽忠 《成都信息工程学院学报》2006,21(4):583-585

在区间值直观模糊集上定义了一系列拓扑空间中的概念，并得到了一些重要结论。  相似文献   

三维GIS的数据结构探讨     

左兴东 《测绘与空间地理信息》2014,(7):120-122

对二维GIS数据结构的缺陷及建立三维GIS数据结构的紧迫性进行了简单阐述,列举了几种常见的三维GIS数据结构,并探讨了如何使用面向对象的方法来构建三维GIS数据结构,针对三维GIS数据结构研究的大体发展趋势做了进一步的阐述。最后提出了有关三维GIS数据结构设计与数据存储方法的一点建议。  相似文献   

油田地面工程拓扑关系建立及展示技术研究     

崔国刚 《测绘与空间地理信息》2014,(5):98-100

重点研究了油田地面工程拓扑关系的建立、更新及展示问题。分析总结出了油田地面工程原油集输系统的拓扑关系,介绍了建立拓扑关系的方法,并提出了通过逻辑示意图把拓扑关系从图形数据转换到属性数据的方法,提高了油田地面拓扑关系的展示效率。  相似文献