首页> 外文期刊>Sedimentology: Journal of the International Association of Sedimentologists >Environmental controls on the development of Mississippian microbial carbonate mounds and platform limestones in southern Montagne Noire (France)
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Environmental controls on the development of Mississippian microbial carbonate mounds and platform limestones in southern Montagne Noire (France)

机译:南蒙古南部密西西比亚微生物碳酸土墩和平台石灰岩的环境控制(法国)

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Late Mississippian carbonates in southern Montagne Noire are dominantly domical to laterally-accreted microbial mounds in some formations, as well as stratiform microbial limestones occurring in hundreds of olistoliths within a flysch basin, constituting pieces of a giant puzzle that are used to help reconstruct a platform in a region that is no longer preserved. Petrographic data of limestone samples from 14 continuous long sections of olistoliths have been analyzed statistically, using multivariate clustering (Q-mode) of the components/matrix/cement and canonical correspondence analysis that allow the reconstruction of the environmental parameters of carbonate microbial communities in space and time. Clustering analysis separated microbial and non-microbial facies. The calculation of indices along the various axes from canonical correspondence analysis allows recognition of the controlling factors of the mounds and microbial growth as being turbidity, light penetration, bathymetry and storms. Turbidity and light penetration are the primary factors controlling the morphology of the microbial limestones. Representation of the light penetration and bathymetry indices on the stratigraphical sections defines two vertical environmental gradients. Light penetration can be subdivided into euphotic, euphotic-dysphotic and dysphotic-aphotic conditions. The representation of the bathymetry allows the subdivision of samples into a deeper outer ramp, external mid-ramp and internal mid-ramp. The curve distance from the section base = f (index) suggests a cyclicity for the platform that cannot be compared with the onlap curve defined from other cratonic areas (Moscow Basin), and thus the cyclic succession of the Montagne Noire is interpreted to have been mostly tectonically-controlled. Integration of the data allowed the reconstruction of the original Mississippian carbonate platform, where, up to the Mikhailovian, it appears to correspond to a platform morphology, with narrow s
机译:南部蒙塔根内的未遂密西西比州碳酸盐在某些地层中横向凸起的微生物丘,以及在鸡球盆中的数百个奥里斯洛斯中出现的层状微生物石灰岩,构成用于帮助重建平台的巨型拼图在不再保留的区域中。已经在统计上分析了来自14个连续长孔的石灰石样本的石灰石样本的岩画数据,使用组件/基质/水泥和水泥和规范对应分析的多元聚类(Q-MODE),其允许重建空间中碳酸盐微生物群落的环境参数和时间。聚类分析分离微生物和非微生物相。沿规范对应分析的各种轴的指数计算允许识别土墩和微生物生长的控制因子,因为浊度,光渗透,沐浴浴和风暴。浊度和光渗透是控制微生物石灰石形态的主要因素。地层部分上的光渗透和沐浴索引的表示定义了两个垂直环境梯度。光渗透可以细分为Euphotic,Euphotic-Dysphotic和Dysphotic-Aphotic条件。浴型的表示允许样品细分成更深的外斜坡,外部中坡和内部斜坡。从截面= f(索引)部分的曲线距离表明平台的循环性与从其他克拉索区域(莫斯科盆地)定义的onlap曲线无法比较,因此蒙特伽群地区的循环连续被解释为主要是针对性控制的。数据集成允许重建原始密西西比碳酸盐平台,在那里,直到米哈伊夫罗维安,它似乎对应于平台形态,狭窄的s

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