首页> 外文学位 >Origin of thorium/uranium variations in chondritic meteorites.
【24h】

Origin of thorium/uranium variations in chondritic meteorites.

机译:软骨陨石中//铀变异的起源。

获取原文
获取原文并翻译 | 示例

摘要

Isotope dilution thorium and uranium analyses of the Harleton chondrite show a larger scatter than previously observed in equilibrated ordinary chondrites (EOC). The linear correlation of Th/U with l/U in Harleton (and all EOC data) is produced by variations in the chlorapatite to merrillite mixing ratio. Apatite variations control the U concentrations. Phosphorus variations are compensated by inverse variations in U to preserve the Th/U vs. l/U correlation. Because the Th/U variations reflect phosphate sampling, a weighted Th/U average should converge to an improved solar system Th/U. We obtain Th/U = 3.53 (1σ mean = 0.10), significantly lower and more precise than previous estimates.; To test whether apatite also produces Th/U variations in CI and CM chondrites, we performed P analyses on the solutions from leaching experiments of Orgueil and Murchison meteorites.; A linear Th/U vs. l/U correlation in CI can be explained by redistribution of hexavalent U by aqueous fluids into carbonates and sulfates.; Unlike CI and EOC, whole rock Th/U variations in CMs are mostly due to Th variations. A Th/U vs. l/U linear correlation suggested by previous data for CMs is not real. We distinguish 4 components responsible for the whole rock Th/U variations: (1) P and actinide-depleted matrix containing small amounts of U-rich carbonate/sulfate phases (similar to CIs); (2) CAIs and (3) chondrules are major reservoirs for actinides, (4) an easily leachable phase of high Th/U, likely carbonates produced by CAI alteration. Phosphates play a minor role as actinide and P carrier phases in CM chondrites.; Using our Th/U and minimum galactic ages from halo globular clusters, we calculate relative supernovae production rates for 232Th/ 238U and 235U/238U for different models of r-process nucleosynthesis. For uniform galactic production, the beginning of the r-process nucleosynthesis must be 13 Gyr. Exponentially decreasing production is also consistent with a 13 Gyr age, but very slow decay times are required (35 Gyr), approaching the uniform production. The 15 Gyr Galaxy requires either a fast initial production growth (infall time constant 0.5 Gyr) followed by very slow decrease (decay time constant >100 Gyr), or the fastest possible decrease (≈8 Gyr) preceded by slow infall (≈7.5 Gyr).
机译:Harleton球粒陨石的同位素稀释th和铀分析显示,其散布比以前在平衡普通球粒陨石(EOC)中观察到的更大。 Th / U与Harleton中的L / U的线性相关性(以及所有EOC数据)是由亚磷灰石与磷灰石混合比的变化产生的。磷灰石的变化控制着铀的浓度。磷的变化通过U的逆变化来补偿,以保持Th / U与l / U的相关性。由于Th / U的变化反映了磷酸盐采样,因此加权的Th / U平均值应收敛到改进的太阳系Th / U。我们获得的Th / U = 3.53(1σ平均值 = 0.10),比以前的估计值低得多,也更精确。为了测试磷灰石是否还会在CI和CM球粒陨石中产生Th / U变化,我们对Orgueil和Murchison陨石的浸出实验溶液进行了P分析。 CI中线性的Th / U与l / U相关性可以通过含水流体将六价U重新分布为碳酸盐和硫酸盐来解释。与CI和EOC不同,CM中整个岩石Th / U的变化主要归因于Th的变化。先前数据对CM提出的Th / U与l / U线性相关不是真实的。我们区分出造成整个岩石Th / U变化的4个成分:(1)P和act系元素贫化的基质,其中含有少量的富含U的碳酸盐/硫酸盐相(类似于CI); (2)CAI和(3)软骨是act系元素的主要储层,(4)高Th / U的易于浸出相,可能是CAI改变产生的碳酸盐。磷酸盐在CM球粒陨石中仅作为act系元素和P载流子相起作用。利用我们的Th / U和来自晕球状星团的最小星系年龄,我们计算出 232 Th / 238 U和 235 U的相对超新星生产率/ 238 U用于不同的r过程核合成模型。为了产生均匀的银河,r过程核合成的开始必须小于13 Gyr。呈指数下降的产量也与13 Gyr年龄一致,但需要非常缓慢的衰减时间(<35 Gyr),接近均匀产量。 15 Gyr星系需要快速的初始产量增长(下降时间常数<0.5 Gyr),然后非常缓慢的下降(衰减时间常数> 100 Gyr),或者可能是最快的下降速度(&ap; 8 Gyr),之后是缓慢的下降(&ap ; 7.5 Gyr)。

著录项

  • 作者

    Goreva, Julia S.;

  • 作者单位

    California Institute of Technology.;

  • 授予单位 California Institute of Technology.;
  • 学科 Geochemistry.
  • 学位 Ph.D.
  • 年度 2001
  • 页码 190 p.
  • 总页数 190
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号