...
首页> 外文期刊>Journal of paleolimnology >Diagenetic sequestration of rare earths and actinides in phosphatic oil shale from the lacustrine Green River Formation (Eocene), Utah, USA: an SEM and LA-ICP-MS study
【24h】

Diagenetic sequestration of rare earths and actinides in phosphatic oil shale from the lacustrine Green River Formation (Eocene), Utah, USA: an SEM and LA-ICP-MS study

机译:犹他州犹他州绿色河流形成(虫族)中磷油页岩的稀土和阳光亢进的成岩依赖性 - SEM和LA-ICP-MS研究

获取原文
获取原文并翻译 | 示例
           

摘要

AbstractThe upper Green River Formation of the eastern Uinta Basin of Utah comprises variably organic-rich mudrock deposited in a stratified, alkaline lake that fluctuated in size and in hydrology from open to evaporitic. Beds of oil shale, representing periods of deep lake, suboxic-anoxic deposition include examples with anomalously high phosphate and toxic trace-metal levels, as determined by whole rock X-ray diffraction, scanning electron microscopy (SEM), and both solution and laser-ablation (LA) inductively coupled plasma-mass spectrometry (ICP-MS). The SEM identifies an early, pre-compaction, diagenetic succession of euhedral rhombic dolomite and high-Mg-calcite, nodular pyrite, blocky low-Mg calcite, and microcrystalline carbonate fluorapatite (CFA). LA-ICP-MS indicates the CFA intervals have distinct lower and upper margins where P content rises from ~0.079 to ~3.2% across 2–3?cm of section. Enrichments of rare earth elements (REEs) and actinides (Th, U) show a complex correlation with the phosphatic margins. Light REEs average a tenfold enrichment at the outer margins with progressively heavier REEs exhibiting up to 20-fold enrichment toward the inner margin (Lu from 0.15 to 2.63?ppm). Actinide abundances also increase tenfold (U from ~5 to ~80?ppm) toward the inner margin. There is greatest similarity between Th and the Ho distributions and between U and Lu. This is a similar distribution to what elsewhere has been found in fossil bone and teeth. The microcrystalline CFA is interpreted to have precipitated (or recrystallized from a precursor phosphate) when the rate of dissolved P being generated from organic-matter breakdown exceeded P diffusion rates into the water column, allowing for P supersaturation. As the crystallites grew, diffusion of REE and actinide ions and complexes from surrounding porewaters into the concreting phosphate occurred only until por
机译:<![cdata [ <标题>抽象 ara id =“par1”> uinta盆地的上绿河形成犹他州包括可变有机富含有机含有有机堆积的浑浊,沉积在分层的碱性湖泊中,其尺寸波动和水性从开放到蒸发液中。油页岩床,代表深层湖泊,中毒缺氧沉积包括具有异常高磷酸盐和有毒痕量金属水平的实例,如全岩X射线衍射,扫描电子显微镜(SEM)和溶液和激光所测定 - 建筑(LA)电感耦合等离子体质谱(ICP-MS)。 SEM鉴定了Euhedral菱形白云石和高Mg-亚铁铝石,结节硫铁矿,块状低Mg方解石和微晶碳酸氟代磷灰石(CFA)的早期,预压缩,乳头成型成绩。 La-ICP-MS表示CFA间隔具有不同的下部和上边缘,其中P含量从2-3°C的截面〜0.079至〜3.2%上升。稀土元素(REES)和散氨酸(TH,U)的富集显示与磷酸盐边距复杂的相关性。光线在外边缘的平均富力富集,逐步较重的REES表现出高达20倍的富集朝向内部边缘(Lu为0.15至2.63μm≤PPM)。滑动性丰富也将十倍(U来自〜5至〜80〜80?ppm)朝内边缘增加。 TH和HO分布之间以及U和LU之间存在最大的相似性。这是在化石骨和牙齿中发现的其他地方的类似分布。当从有机物质击穿产生的溶解P速率超过P扩散速率进入水柱时,将微晶CFA解释为沉淀(或从前体磷酸盐重结晶),允许p过饱和。随着微晶的增长,REE和致散性离子的扩散和从周围的苦汗进入混凝土磷酸盐的络合物发生直到por发生

著录项

相似文献

  • 外文文献
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