Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1130/B35174.1 |
Diagenetic to incipient metamorphic zones of the Benton Uplift, Ouachita Orogen, Arkansas, USA | |
Johnson, Harold E., II1; Wiltschko, David, V1; Harris, John P.2 | |
2020-05-01 | |
发表期刊 | GEOLOGICAL SOCIETY OF AMERICA BULLETIN
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ISSN | 0016-7606 |
EISSN | 1943-2674 |
出版年 | 2020 |
卷号 | 132期号:5-6页码:977-986 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | Vitrinite reflectance analysis and the mean diameter of metamorphosed quartz, suggest that the eastern Ouachita region, Arkansas, USA reached the lower greenschist facies, regardless of burial depth. An increase in "crystallinity" may explain that the maturation is from the exhumation of the rocks from a greater depth. Shale and sandstone samples collected from outcrops along the crest of the Benton Uplift exhibit illite and chlorite crystallinities that yield higher indices compared to younger rocks adjacent to this crustalscale anticlinal structure. Illite crystallinity d(001) of air-dried, fine (<0.2 mu m) authigenic clays (Delta degrees 2 circle minus (CuK alpha) = 0.417 degrees to 0.875 degrees) yield a range of conditions from diagenetic temperature to lower anchizone temperatures up to -200 degrees C. Air-dried, fine authigenic chlorite clays (Delta degrees 2 circle minus (CuK alpha) = 0.259 degrees to 1.570 degrees) yield a wide range of diagenetic to metamorphic conditions that span the diagenetic zone through epizone, which indicate a maximum temperature slightly above similar to 300 degrees C. These results are in contrast to prior thermal maturation data. No additional heat sources, such as from pluton emplacement, were identified by major areas of anomalous high maturation based on crystallinity. Regionally, the illite and chlorite crystallinity increases to-ward the central axis of the Benton Uplift. Exhumation of the rocks from greater depth is all that is required to explain the illite and chlorite crystallinity data. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000530917400006 |
WOS关键词 | X-RAY-DIFFRACTION ; ILLITE CRYSTALLINITY ; VITRINITE REFLECTANCE ; CARBONIFEROUS STRATA ; ARKOMA BASIN ; MOUNTAINS ; OKLAHOMA ; CHLORITE ; ALPS |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/279472 |
专题 | 地球科学 |
作者单位 | 1.Texas A&M Univ, Dept Geol & Geophys, Ctr Tectonophys, 3115 TAMU, College Stn, TX 77843 USA; 2.Sam Houston State Univ, Dept Geog & Geol, POB 2148, Huntsville, TX 77341 USA |
推荐引用方式 GB/T 7714 | Johnson, Harold E., II,Wiltschko, David, V,Harris, John P.. Diagenetic to incipient metamorphic zones of the Benton Uplift, Ouachita Orogen, Arkansas, USA[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2020,132(5-6):977-986. |
APA | Johnson, Harold E., II,Wiltschko, David, V,&Harris, John P..(2020).Diagenetic to incipient metamorphic zones of the Benton Uplift, Ouachita Orogen, Arkansas, USA.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,132(5-6),977-986. |
MLA | Johnson, Harold E., II,et al."Diagenetic to incipient metamorphic zones of the Benton Uplift, Ouachita Orogen, Arkansas, USA".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 132.5-6(2020):977-986. |
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