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首页> 外文期刊>Rocky Mountain Geology >Revisions to stratigraphic nomenclature of the Upper Triassic Chinle Group in New Mexico: New insights from geologic mapping, sedimentology, and magnetostratigraphic/paleomagnetic data
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Revisions to stratigraphic nomenclature of the Upper Triassic Chinle Group in New Mexico: New insights from geologic mapping, sedimentology, and magnetostratigraphic/paleomagnetic data

机译:新墨西哥州上三叠纪Chinle组地层命名的修订:地质制图,沉积学和地磁/古地磁数据的新见解

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摘要

Upper Triassic strata, termed the Chinle Formation or Group, reveal a complex sedimentologic history, which has led to numerous modifications to the lithostratigraphic nomenclature for this unit. Recent revisions to Chinle nomenclature in New Mexico are based on local stratigraphic section inspection. The utility of some stratigraphic subdivisions, especially at formation rank, are problematic when mapping units away from type areas. New magnetostratigraphic records for the Chinle Group, as well as 1:24,000-scale mapping, stratigraphic section logs, and sedimentologic analyses support the following revisions to current nomenclature of the Chinle: (1) formally raising Chinle strata to group status in New Mexico; (2) abandoning the term Zuni Mountains Formation for lower Chinle strata in the Chama Basin; (3) including the lower member of the Salitral Formation in the Shinarump Formation; and (4) reassigning strata termed Rock Point Formation in the Chama Basin to the Moenave Formation. Sedimentologic and basin-analysis interpretations utilized in earlier studies of the Chinle should be resurrected. The revised stratigraphic nomenclature for the Chinle Group and sedimentologic analyses, both old and new, greatly expands our understanding of depositional changes in the Chinle Basin of northern New Mexico. The trunk stream for Chinle deposition in New Mexico coursed westward through the site of the modern Sierra Nacimiento of north-central New Mexico during Shinarump time (?late Carnian or early Norian), then moved northward to flow to the west in the area of the modern Chama Basin. In addition, north-central New Mexico was probably a topographic high during the time of Owl Rock and Rock Point deposition in the late Norian, and thus no uppermost Triassic (late Norian to early Rhaetian) strata were deposited in the area of the modern Chama Basin.
机译:上三叠世地层,被称为Chinle组或组, 揭示了一个复杂的沉积历史,这导致对该 的岩石地层学术语进行了许多 修改。单元。新墨西哥州 对Chinle术语的最新修订基于当地地层剖面检查。当将单位远离类型区域映射时,某些地层细分的效用 尤其是在地层 等级时是有问题的。 Chinle组的新地磁记录,以及 以及1:24,000比例尺的制图,地层剖面测井和沉积学 分析都支持对Chinle当前的命名法 进行以下修订: (1)在新墨西哥州正式将Chinle阶层提升为团体状态 ; (2)放弃Chama盆地下Chinle地层的祖尼山脉组 ; (3)包括Shinarump组中盐岩组的 下层成员; 和(4)重新分配Chama中 的岩点组盆地至莫埃纳夫组。应当对在Chinle早期研究中使用的沉积学和盆地分析 解释进行复活。修订后的 Chinle组的地层命名法和新旧的 沉积学分析极大地扩展了我们对 Chinle盆地沉积变化的认识新墨西哥州北部。在新纳伦时期,新墨西哥州 沉积沉积的干流向西穿过新墨西哥州中北部现代塞拉纳西门托(Sierra Nacimiento)的 站点向西移动(到晚Carnian或Norian早期),然后 向北移动到现代 Chama盆地的区域向西流动。另外,在诺里安晚期猫头鹰岩和Rock Point 沉积时期,新墨西哥州中北部可能是 地形高点,因此没有最高的三叠纪 (诺里安晚期至拉蒂安早期)地层沉积在现代Chama盆地的 区域。

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  • 来源
    《Rocky Mountain Geology》 |2008年第2期|121-141|共21页
  • 作者单位

    Department of Earth and Planetary Sciences, Northrop Hall MSC 03-2040, University of New Mexico, Albuquerque, New Mexico 87131, U.S.A.;

    New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech University, 801 Leroy Place, Socorro, New Mexico 87801, U.S.A.;

    Department of Earth and Planetary Sciences, Northrop Hall MSC 03-2040, University of New Mexico, Albuquerque, New Mexico 87131, U.S.A.;

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