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The Steens Basalt of the Oregon Plateau: A geomagnetic polarity reversal and the age of the Columbia River basalt group.

机译:俄勒冈高原的Steens玄武岩:地磁极性反转和哥伦比亚河玄武岩群的年龄。

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摘要

The Steens Basalt of the Oregon Plateau covers about 53,000 km2 of southeastern Oregon and northwestern Nevada. Three localities where volcanic sections contain transitional lavas of the Steens reversal have been studied. At Steens Mountain, previous studies showed a complex reversal path consisting of 30 transitional directional groups. At the three new localities, forty-five new transitional directional groups are discovered, show an increase in the complexity of the reversal path, and reinforce the clumping of some directions. Fifteen 40Ar/39Ar ages were determined from lavas on or near the Oregon Plateau. The lavas are shown to have erupted before, after, or during the Steens reversal in the R0, N 0, or N1 of the CRBG. Using a Bayesian statistical analysis of the mean age of the Steens reversal lavas and three other ages at the Catlow section, the best and preferred age of the Steens reversal is 16.73 +0.13/-0.08 Ma (95% confidence). Correlation of this age to a sea floor spreading time scale allows the floating magnetostratigraphy of the CRBG to be placed into the geomagnetic polarity time scale and shows that the R0 corresponds to the C5Cr chron with the Steens reversal at the top of the C5Cr chron. Twenty six paleomagnetic poles from Steens Mountain are combined with 108 non-transitional poles found in this thesis to give a clockwise rotation of the Oregon Plateau of 11.4° +/- 5.6° with respect to the younger CRBG flows to the north and 14.5° +/- 4.6° with respect to cratonic North America. Using secular variation considerations, eruption rates can be calculated at two of the sections which contain the Steens reversal: 85--120 m/ka at Catlow and 130--195 m/ka at Poker Jim South. Similarly, durations of eruptions have been determined at the four sections that do not contain the Steens reversal: &sim2.5 ka for 260 m at the Pueblo Mountains, 0.5 to 1.5 ka for 190 m at Summit Springs, 1--3 ka for 170 m at North Mickey, and &sim3 ka for 160 m at Guano Rim.
机译:俄勒冈高原的Steens玄武岩覆盖了俄勒冈州东南部和内华达州西北部约53,000 km2。已经研究了三个火山段包含斯坦斯逆转过渡熔岩的地方。在Steens Mountain,先前的研究显示了由30个过渡方向组组成的复杂的反向路径。在这三个新地点,发现了四十五个新的过渡方向组,它们显示出反向路径的复杂性增加,并加强了某些方向的聚集。从俄勒冈高原上或附近的熔岩中确定了15个40Ar / 39Ar年龄。结果表明,在CRBG的R0,N 0或N1发生Steens反转之前,之后或期间,熔岩已经喷发。通过对Stelow逆转熔岩的平均年龄和Catlow断面的其他三个年龄的贝叶斯统计分析,Steens逆转的最佳和首选年龄为16.73 + 0.13 / -0.08 Ma(95%置信度)。这个年龄与海床扩展时间尺度的相关性使得CRBG的浮磁地层学可以被放置到地磁极性时间尺度中,并且表明R0对应于C5Cr年代,而Steens逆转位于C5Cr年代的顶部。将来自Steens Mountain的26个古磁极与本论文中发现的108个非过渡极相结合,使俄勒冈高原的顺时针方向相对于向北流的年轻CRBG顺时针旋转为11.4°+/- 5.6°,而对于北向的CRBG顺时针旋转为14.5°+ /-关于克拉通北美地区为4.6度。使用长期变化考虑因素,可以在包含Steens反转的两个部分中计算喷发率:卡特隆(Catlow)为85--120 m / ka,扑克吉姆南(Poker Jim South)为130--195 m / ka。同样,在不包含Steens逆转的四个部分确定了喷发的持续时间:普韦布洛山脉(Sue)的&sim2.5 ka(260 m),Summit Springs(190 m)的0.5至1.5 ka(190 m),170(170)的1--3 ka米在北米奇(North Mickey)处,&sim3 ka在160米处(Guino Rim)。

著录项

  • 作者

    Jarboe, Nicholas A.;

  • 作者单位

    University of California, Santa Cruz.;

  • 授予单位 University of California, Santa Cruz.;
  • 学科 Geology.Geophysics.
  • 学位 Ph.D.
  • 年度 2010
  • 页码 187 p.
  • 总页数 187
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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