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派生裂隙
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     The tin ore zone is restricted by the second-order fractures of the Lianhuashan fault belt, and the ore deposits and orebodies mainly occur along the NE-NEE interlayer-gliding fractures and their derivative fissures, showing structural positioning features.
     锡矿带受莲花山断裂带的次一级断裂制约,矿床、矿体主要产于NE-NEE向层间滑动断裂及其派生裂隙中,锡矿具有构造定位的特征。
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     Slit Lamps
     裂隙
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     Infixation: from Inflectional to Derivational
     中缀:从屈折到派生
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     Shareholders Derivative Suit
     股东派生诉讼
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     The development of a slit_lamp fluorophotometer
     裂隙灯荧光光度计
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     With the proceed of the shearing, the conjugated tension fractures are derived,which provides once more the space for ore accumulation.
     随着剪切作用的持续进行,派生了里德尔共轭裂隙,再次为金矿化提供了容矿空间。
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A model is proposed for the process of laser-induced fracture in transparent dielectrics.
      
Thermal stress-induced fracture of coating layer of galvannealed steel
      
The inflow is localized by natural and induced fracture zones and is mostly into recent workings.
      
In this work, we collect and observe particles produced from single-crystal sodium nitrate during irradiation at 1.06?μm as a function of fluence and explore the possibility that laser-induced fracture may produce suitable particles.
      
High-power diode-end-pumped Nd:YVO4 laser: thermally induced fracture versus pump-wavelength sensitivity
      
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The tin ore deposits(occurrences) in Changpu-Jishuimen tin ore zone almost unexceptionally occur in 2nd subgroup of Lower Jurassic Jinji Group. The distribution pattern of the tin ore zone and the shape and mode of occurrence of orebodies indicate that the ore deposits are controlled by the stratigraphic horizon. The tin ore zone is restricted by the second-order fractures of the Lianhuashan fault belt, and the ore deposits and orebodies mainly occur along the NE-NEE interlayer-gliding fractures and their derivative...

The tin ore deposits(occurrences) in Changpu-Jishuimen tin ore zone almost unexceptionally occur in 2nd subgroup of Lower Jurassic Jinji Group. The distribution pattern of the tin ore zone and the shape and mode of occurrence of orebodies indicate that the ore deposits are controlled by the stratigraphic horizon. The tin ore zone is restricted by the second-order fractures of the Lianhuashan fault belt, and the ore deposits and orebodies mainly occur along the NE-NEE interlayer-gliding fractures and their derivative fissures, showing structural positioning features. The ore deposits generally underwent early and late metallogenic epochs, the first one taking place before the late Jurassic volcanism and the second at the end of Jurassic to Early Cretaceous. The ore-forming substances came from several sources but mainly from the strata. The Jinji Group was enriched in tin and some other metallogenic elements and thus served as an important source bed. The ore-forming solutions were mainly metamorphous water which however was mixed with some meteoric water. The tin deposits are of sedimentary-metamorphogenic stratabound type.

广东长埔—吉水门锡矿带内的锡矿床(点)几乎毫无例外地赋存于下侏罗统金鸡群第二亚群中,锡矿带的展布格局和矿体的形态、产状等特征说明,锡矿受地层层位控制。锡矿带受莲花山断裂带的次一级断裂制约,矿床、矿体主要产于NE-NEE向层间滑动断裂及其派生裂隙中,锡矿具有构造定位的特征。矿床一般经历了早、晚两个成矿期,第一成矿期发生于晚侏罗世火山作用之前,第二成矿期形成于晚侏罗世末期至早白垩世。成矿物质是多来源的,但主要来自地层。金鸡群地层富含锡等成矿组分,是重要的矿源层。成矿溶液以变质水为主,并有大气降水混入。锡矿床属沉积-变成层控矿床。

There are a lot of lodes of east west trend in Hunan,many of them forming large scal deposits,thus being of important economic value.The distribution of these lodes is in connection with the ductile shear zones of northeastern trend and their induced fissures.The belts along and nearby these ductile shear zones is the propecting direction.

在湖南境内有许多东西走向和接近东西走向的矿脉,不少矿脉具有大型矿床规模,有重要的经济价值。这类矿脉(床)的分布,大都与北东走向的韧性剪切带及其派生的裂隙系统有关,沿此种剪切带及其旁侧,是今后的找矿方向。

According to the recent survey evaluation and integrated study of mineral resources in South China,this paper summaries the characteristics of structural control of ore deposition at different spatial levels,from the lithosphere to microfracture networks,including deep lithosphere delamination and thinning and related geodynamic regime transition of tectono-metallogonic domains→control of distribution of metallogenic belts (ore concentration areas) by regional tectonic thinning zones and related alkali-rick...

According to the recent survey evaluation and integrated study of mineral resources in South China,this paper summaries the characteristics of structural control of ore deposition at different spatial levels,from the lithosphere to microfracture networks,including deep lithosphere delamination and thinning and related geodynamic regime transition of tectono-metallogonic domains→control of distribution of metallogenic belts (ore concentration areas) by regional tectonic thinning zones and related alkali-rick (A-type) mogma assoications→control of distribution of small (porphyry) rock bodies and related ore fields (deposits) by structural compounding loci→control of occurrence of orebodies by major faults and their associated and derivative fracture networks→control of concentration of ore substances by dynamic transition of structure deformation and related hydrofracturing.It put special emphasis on the dominant role that tensile structural systems of different scales related to mesozoic lithospheric delamination play in controlling ore deposition.This has great significance for the metallogenic analysis and mineral exploration.

根据华南地区近期矿产资源调查评价及综合研究资料,本文简要总结从岩石圈至微破裂网络等不同层次构造控矿特征,包括深部岩石圈拆沉减薄及相关的构造成矿(域)动力学体制转换→区域构造减薄带及相关富碱(A型)岩浆组合控制区域成矿带(矿集区)展布→构造复合部位控制小(斑)岩体及相关的矿田(床)分布→主干断裂及圈闭组合有关的伴生、派生裂隙网络控制矿体产出→构造变形动力学转换及相关水压致裂控制矿质富集等,特别强调与中生代岩石圈拆沉作用相关的不同尺度张性构造系统的控矿主导作用,这对于华南地区区域成矿分析和矿产勘查均具有重要意义。

 
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