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甘肃礼岷金矿田的中继构造及其控矿作用 被引量:3
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作者 奚小双 张曾荣 《矿产与地质》 1995年第1期33-37,共5页
对甘肃礼岷金矿田控矿断裂的组合形式和力学性质的分析表明具有中继构造的模式,矿体为正断层带,呈不连续的错位排列,错位矿体的排列型式受基底构造控制,矿体的构造变形软弱,显示了断层带发展初期的特征。矿体在深部有规模扩大的趋... 对甘肃礼岷金矿田控矿断裂的组合形式和力学性质的分析表明具有中继构造的模式,矿体为正断层带,呈不连续的错位排列,错位矿体的排列型式受基底构造控制,矿体的构造变形软弱,显示了断层带发展初期的特征。矿体在深部有规模扩大的趋势,与控矿断裂从深部向浅部的扩展顺序有关,这是岩体外接触带构造环境和矿液压裂作用的结果。 展开更多
关键词 中继构造 错位断裂 金矿床 控矿作用
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正断层中继构造扩展演化机制及对成矿构造研究的启示
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作者 汤静如 奚小双 +3 位作者 李欢 李文光 曾南石 赵义来 《大地构造与成矿学》 EI CAS CSCD 北大核心 2019年第3期507-517,共11页
正断层的分段构造型式及其扩展演化机制的核心内容可以归结为正断层的中继构造模式。本文从正断层的断块变形、断裂扩展以及断裂力学特征等角度,总结了正断层中继构造的扩展演化机制。正断层的断块变形是指分段断层位移转换形成的中继斜... 正断层的分段构造型式及其扩展演化机制的核心内容可以归结为正断层的中继构造模式。本文从正断层的断块变形、断裂扩展以及断裂力学特征等角度,总结了正断层中继构造的扩展演化机制。正断层的断块变形是指分段断层位移转换形成的中继斜坡,可分为内倾和外倾两种斜坡类型,位移曲线揭示了中继带变形的特征。正断层的断裂扩展有多种扩展方式,可分为断层内、断层间和断层系扩展,且可以形成不同型式的中继构造。正断层中继构造是在三维空间扩展的,将断层边缘的断裂力学性质和断层面的放射状扩展方向相结合,可完整描述中继构造的空间分布规律。正断层形成于伸展构造环境,是控制油气和金属矿产资源的重要构造型式,结合SEDEX型矿床同生断层和岩体侵位控制的正断层控矿研究实例,初步讨论了正断层中继构造扩展演化在SEDEX型矿床和正断层相关控矿断裂成矿构造研究中的作用。 展开更多
关键词 正断层中继构造 中继斜坡 断层扩展演化 成矿构造
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Practical Polar Code Construction For Degraded Multiple-Relay Networks 被引量:2
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作者 Bin Duo Xiaoling Zhong Yong Guo 《China Communications》 SCIE CSCD 2017年第4期127-139,共13页
In this paper, based on the characteristics of polar codes, a new decode-and-forward strategy called generalized partial information relaying protocol is proposed for degraded multiple-relay networks with orthogonal r... In this paper, based on the characteristics of polar codes, a new decode-and-forward strategy called generalized partial information relaying protocol is proposed for degraded multiple-relay networks with orthogonal receiver components(MRNORCs). In such a protocol, with the help of partial information from previous nodes, each relay node tries to recover the received source message and re-encodes part of the decoded message for transmission to satisfy the decoding requirements for the following relay node or the destination node. In order to construct practical polar codes, the nested structures are developed based on this protocol and the information sets corresponding to the partial messages forwarded are also calculated. The proposed scheme is proved to be capable of achieving the theoretical capacity of the degraded MRN-ORCs while still retains the low-complexity feature of polar codes. We perform simulations to testify the practicability of the proposed scheme and compare polar codes by using successive-cancellation list decoder(SCLD) with traditional low-density parity-check(LDPC) codes. The results show that the obtained polar codes provide significant gain. 展开更多
关键词 cooperative communication multiple-relay networks channel capacity decode-and-forward polar codes
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Heterogenous zircons from Mesozoic igneous rocks in the North China Craton and their tectonic implications
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作者 MIAO Laicheng FAN Weiming +1 位作者 ZHANG Fuqin LIU Dunyi 《Global Geology》 2009年第3期122-133,共12页
Based on a synthesis of zircon inheritance from Mesozoic igneous rocks in the eastern portion of the North China Craton (NCC) , it is proposed that inherited zircons with Neoproterozoie ages identified from these ro... Based on a synthesis of zircon inheritance from Mesozoic igneous rocks in the eastern portion of the North China Craton (NCC) , it is proposed that inherited zircons with Neoproterozoie ages identified from these rocks are of a heterogenous derivation from the Yangtze/South China block, rather than from the NCC itself. The mechanism that introduces these zircons incorporated into the NCC is likely by tectonic underplating during the Triassic continental subduction of the Yangtze block beneath the NCC. Tectonic addition of abundant crustal materials represented by the heterogenous zircons into the NCC, probably along Moho or weak interfaces within the NCC's crust, led to the crustal thickening in the NCC. These heterogenous materials, either as (partial) source rocks or as contaminants of the magmas generated during an extension environment following the crustal thickening, were reworked and therefore have significant contribution to petrogenesis of the Mesozoic igneous rocks. The crustal thickening resulted from the tectonic underplating, as indicated by the distribution extent of the heterogenous zircons, is spatially similar to that of the lithospheric thinning, with both mainly occurring in the eastern segment of the NCC. This is probably suggestive of an intrinsic relation between the thickening and thinning events during the Mesozoic evolution of the NCC. 展开更多
关键词 inherited zircon igneous rock NEOPROTEROZOIC MESOZOIC North China Craton
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