AbstractA 1248 m long core (KBH 07, 17°18′07″ N; 73°47′28.2″E, 960m above msl) drilled up to basement in the Deccan traps from Koyn'/> Magnetic mineralogical variability along Deccan trap basalt borehole (KBH07), Koyna deep continental drilling program, western Maharashtra, India
首页> 外文期刊>Journal of the Geological Society of India >Magnetic mineralogical variability along Deccan trap basalt borehole (KBH07), Koyna deep continental drilling program, western Maharashtra, India
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Magnetic mineralogical variability along Deccan trap basalt borehole (KBH07), Koyna deep continental drilling program, western Maharashtra, India

机译:沿甲板陷阱玄武岩钻孔钻孔(KBH07),Koyna Deep Continental钻井计划,印度西部马哈拉施特拉邦的磁性矿物学可变性

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AbstractA 1248 m long core (KBH 07, 17°18′07″ N; 73°47′28.2″E, 960m above msl) drilled up to basement in the Deccan traps from Koyna region was sampled at ~10m interval for magnetic mineralogical studies.Analysis of routine rock magnetic parameters (mass specific magnetic susceptibility: χlf, frequency dependence of susceptibility: χfd, susceptibility of anhysteretic remanance: χARM, saturation isothermal remanance: SIRM, remanance coercivty: B(0)CR, SoftIRM, HardIRM, S-Ratio, SIRM/χlf, χARMlf) and density (σ, gm/cc) depicted significant higher order temporal variation. The χlfvaries between 13 and 309 x 10-8m3/kg and is independent of density variation. The χARM, B(0)CRand S-Ratios indicate majority of SD-PSD ferrimagnets with episodes of MD ferrimagnetic concentration and few hard coercivity components. The giant plagioclase lath bearing (GPB) horizons show highest variability of ferrimagnetic concentration marked by anomalous peaks. Overall the variability of rock magnetic parameters independent of lava flow units suggest that the changeover in magnetic mineral concentration, composition and domain size occur at major episodes in magma composition (e.g., primary source, crustal contamination and fractional crystallization). The studied parameters are therefore examined to mark intervals of (i) magma compositional changes, (ii) zones of oxidative conditions and (iii) rapid/slow cooling intervals demanding detailed petrologic studies. We identified one I order trend, four II order cycles and eight III order cycles for the purpose of correlation. Notable peak in χlfat 650–700m, the chan
机译:<![cdata [ <标题>抽象 ara>一个1248 m长核心(kbh 07,17°18'07“n; 73°47'在磁矿物学研究的〜10M间隔中对来自Koyna地区的Deccan陷阱中钻到地下室的“e,960米以上的MSL)被取样。常规岩石磁性参数分析(质量特定磁敏度:χ<下标> LF ,易感性的频率依赖性:χ<下标> FD ,无间隙剩余的易感性:χ<下标>手臂,饱和等温剩余:SARM,refanance Coercivty:B <下标>(0)Cr < /下标>,软<下标> IRM ,硬<下标> IRM ,S比,SIRM /χ<下标> LF ,χ<下标> ARM / χ<下标> LF )和密度(σ,gm / cc)描绘了显着的高阶时间变化。 χ<下标> LF 在13到309×10-8m3 / kg之间变化,并且与密度变化无关。 χ<下标>臂,B <下标>(0)Cr 和S比标记大多数SD-PSD FerrimaGNET,具有MD亚铁磁性浓度和少量硬矫顽力分量。巨型Plagioclase Lath轴承(GPB)视野显示出由异常峰标记的亚铁磁性浓度的最高可变性。总体而言,独立于熔岩流量单位的岩石磁性参数的可变性表明磁性矿物质浓度,组成和畴尺寸的转换在岩浆组合物(例如,主要源,地壳污染和分数结晶)中发生。因此,研究了研究的参数标记(i)岩浆组成变化的间隔,(ii)氧化条件的区域和(iii)的快速/缓慢冷却间隔要求详细的探测器。我们确定了一个I订单趋势,四个II级循环和八一三III订单周期,以便相关。 χ<下标> lf 在650-700m,陈

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