4.7 Article

Mid-Miocene rhyolite volcanism in northeastern Nevada: The Jarbidge Rhyolite and its relationship to the Cenozoic evolution of the northern Great Basin (USA)

期刊

GEOLOGICAL SOCIETY OF AMERICA BULLETIN
卷 126, 期 7-8, 页码 1047-1067

出版社

GEOLOGICAL SOC AMER, INC
DOI: 10.1130/B30736.1

关键词

-

资金

  1. National Science Foundation (NSF) [EAR-0838139]
  2. NSF [EAR-0838208, EAR-0929991]
  3. NSF GK-12 Program grant [NSF DGE-0841414]
  4. Kansas State University
  5. NASA Space Grant Consortium
  6. Directorate For Geosciences
  7. Division Of Earth Sciences [0838139] Funding Source: National Science Foundation

向作者/读者索取更多资源

We present new physical, geochemical, geochronologic, and oxygen isotope constraints on the mid-Miocene Jarbidge Rhyolite in northeastern Nevada (USA), providing new constraints on the tectonomagmatic evolution of the Cenozoic northern Great Basin. Widespread extension due to rapid collapse of the Nevadaplano began at ca. 17-16 Ma across the northern Great Basin. Coeval with this event was compositionally bimodal basalt-rhyolite volcanism that is often attributed to the inception of the Yellowstone hotspot. The most widespread mid-Miocene volcanic units in northeastern Nevada are lavas and domes of the Jarbidge Rhyolite. The thickest and most areally extensive exposures of these lavas include, and are found just west of, the Jarbidge Mountains, Nevada. This study focuses on Jarbidge Rhyolite directly south of the central Snake River Plain, adjacent to the thickest exposures in the vicinity of Jarbidge, Nevada. Textures on a range of scales indicate that the Jarbidge Rhyolite consists primarily of phenocryst-rich lavas. Laser 40Ar/39Ar ages for sanidine are consistent with effusive eruption of metaluminous to slightly peraluminous ferroan calc-alkalic rhyolite from 16.1 to 15.0 Ma; prior K-Ar ages suggest that some activity occurred over a slightly longer duration. Major and trace element data, coupled with new stable and prior radiogenic isotope measurements, suggest that Jarbidge Rhyolite magmas formed primarily via melting of quartzofeldspathic crust. The Jarbidge Rhyolite lavas are geochemically dissimilar from younger Snake River Plain rhyolites (e. g., lower MgO, lower Nb, higher Rb/Nb) and are more similar to coeval rhyolites erupted to the west on or adjacent to the Oregon Plateau. The distribution of the Jarbidge Rhyolite lavas in northeastern Nevada reflects an intimate association with temporally and spatially coincident extension rather than the Yellowstone hotspot.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据