首页> 外文期刊>Archaeometry >END - MEMBER MIXING ANALYSIS (EMMA) APPLIED TO SEDIMENT GRAIN SIZE DISTRIBUTIONS TO CHARACTERIZE FORMATIONAL PROCESSES OF THE MAIN EXCAVATION BLOCK, UNIT 2, OF THE RIMROCK DRAW ROCKSHELTER (35HA3855), HARNEY BASIN, EASTERN OREGON (USA)
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END - MEMBER MIXING ANALYSIS (EMMA) APPLIED TO SEDIMENT GRAIN SIZE DISTRIBUTIONS TO CHARACTERIZE FORMATIONAL PROCESSES OF THE MAIN EXCAVATION BLOCK, UNIT 2, OF THE RIMROCK DRAW ROCKSHELTER (35HA3855), HARNEY BASIN, EASTERN OREGON (USA)

机译:末端成员混合分析(EMMA)应用于沉积物粒度分布,以表征主要挖掘块的形成过程,牛罗克·罗克斯库尔(35HA3855),牛排,东俄勒冈州(美国)

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摘要

End-member mixing analysis (EMMA) was conducted on the grain size distributions (GSD) of 13 sediment samples collected from the main excavation block, Unit 2, of the Rimrock Draw Rockshelter, a deeply stratified, multi-component Palaeoindian rockshelter in the Harney Basin of eastern Oregon, USA. EMMA confirmed the three stratigraphic units (SU) observed in the field and identified three sedimentary end- members (EM) that account for 95.52% of Unit 2 site formation. EM 1 comprises 70.72% of the total measured grain-size variation and represents fluvial deposition, correlating with the bottom stratigraphic unit, SU 3. EM 2 comprises an additional 17.74% of the total measured grain-size variation and represents fluvially reworked aeolian deposition, correlating with the upper stratigraphic unit, SU 1. EM 3 comprises the remaining 7.06% of the total measured grain-size variation and represents possibly a two-component aeolian deposition of suspension and short-term saltation, correlating with the middle unit, SU 2. The results presented demonstrate the ability of EMMA as a technique to (1) unbiasedly distinguish between the SUs identified in the field using only the measured grain size distributions, (2) provide genetically meaningful and quantitative grain-size end-members to identify multiple major depositional processes of site formation, and (3) provide a geologically meaningful interpretation of site formation that is capable of facilitating the formulation of more focused hypotheses regarding human and environment interactions at the site.
机译:在从主要的挖掘块,13个沉积物样品中,在从主挖掘块,单元2,r rock的粒子2中收集的13个沉积物样品的晶粒尺寸分布(GSD)进行了晶粒尺寸分布(GSD),是哈尼尼的深层分层的多组分帕拉诺印欧岩石美国东部的盆地,美国。艾玛证实了在现场观察到的三个地层单位(SU),并确定了三个沉积终成员(EM),占第2单位形成的95.52%。 EM 1包含总测量粒度变化的70.72%,并且代表氟沉积,与底部地层单元相关,SU 3. EM 2包含总测量的晶粒尺寸变化的另外的17.74%,并且代表氟化物劣化的天气沉积,与上层单位的相关性,SU 1. EM 3包含总测量晶粒尺寸变化的剩余7.06%,并且代表了可能是悬浮液和短期盐化的双组分海洋沉积,与中间单元相关,SU 2相关。所提出的结果证明了EMMA作为技术的能力(1)仅使用测量的晶粒尺寸分布,(2)提供遗传有意义和定量晶粒尺寸的最终成员来识别多个场地地层的主要沉积过程和(3)提供了对能够促进的地质形成的地质有意义的解释制定更多关于现场人和环境相互作用的更焦点假设。

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