(伊朗中部)晚拉丹-早卡尼-阿申组的相分析、沉积环境和地球化学

IF 1 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Payman Rezaee, M. Khanehbad, Moasoumeh Ezatifar, Sayedeh Akram Jooybari, K. Hosseini
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引用次数: 0

摘要

本研究旨在研究晚三叠世Ashin组(伊朗中部Nakhlak群)的岩相、地球化学特征和沉积相。为此,分析了100个薄片和13个细粒沉积岩样本的岩相和地球化学特征,这些样本取自该地层330米厚的剖面。该地层中确定的岩相类型包括砂岩、粉砂岩和石灰岩。研究表明,远海底扇上部向海岸沉积有石灰岩相,中部向海岸沉积砂岩相,下部向深海平原沉积有页岩相。在用于成分分类的三元图上绘制的岩相数据说明了它们的成分为岩屑砂岩、亚岩屑砂岩以及一些岩屑砂岩长石和页岩。离散图是指大陆弧复合体和活动大陆边缘的构造背景。模态分析和地球化学数据的结果表明,这些矿床存在造山再循环。CIA和CIW指数表明源区在半干旱至半湿润气候下具有中等风化作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Facies Analysis, Depositional Environments and Geochemistry of the Late Ladinian-Early Carnian Ashin Formation, (Central Iran)
The present study aims to investigate the petrographic, geochemical features, and depositional facies of the Late Triassic Ashin Formation (Nakhlak Group, central Iran). For this purpose, 100 thin sections, and 13 samples of fine-grained sedimentary rocks were analyzed for their petrographic and geochemical characteristics, taken from a 330-m thick section of this formation. The petrographic types identified in this formation include sandstone, siltstone and limestone. This study suggests limestone facies are deposited in upper parts of the distal submarine fan towards the shore, sandstone facies are deposited in the middle part of the distal submarine fan, and the shale facies are deposited in lower parts of the distal submarine fan towards the abyssal plain by turbidity currents. The plotting of petrographic data on ternary diagrams for compositional classification illustrate their composition as litharenites, sub-litharenites, and a few litharenite-feldspathic and shales. Discrete diagrams refer to a tectonic setting of a continental arc complex and the active continental margin. The results of the modal analysis and geochemical data indicate the orogenic re-cycling for these deposits. CIA and CIW indexes indicate moderate weathering of the source area under semi-arid to semi-humid climates.
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来源期刊
Iranian Journal of Earth Sciences
Iranian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
12.50%
发文量
0
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