太白山盆地龙潭组奥陶纪旌善层新地层方案和层序地层分析及盆地几何学讨论

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Geosciences Journal Pub Date : 2024-03-12 DOI:10.1007/s12303-024-0005-5
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引用次数: 0

摘要

摘要 根据对新近出露、变形较小、相对连续的露头进行的详细沉积学和地层学研究,以及对以往研究的全面回顾,新建立了龙潭组的岩石地层学,主要侧重于在空间和地层上占据龙潭组大部分的贞善层。龙潭组从高到低依次分为旌善层、幸前层和会东里层,所有单元均归入奥陶系。旌善地层根据岩性分为三个单元。旌善地层共有 11 个沉积面,分为五个面系(FA):FA1(滩涂)、FA2(内斜坡)、FA3(浅滩)、FA4(中斜坡)和 FA5(斜坡至外斜坡)。根据解释,该地层沉积于同轴斜坡上。龙潭组被划分为两个超序,以第 1 型序列边界分隔,贞善地层的中下部成员属于超序 I,上部成员属于超序 II,其中包括 Haengmae 和 Hoedongri 地层。根据层序地层分析推断出的相对海平面曲线表明,该地层根据二阶海平面变化经历了两个沉积阶段,以Sauk层序和Tippecanoe层序的边界为分界,该曲线与Taebaek组和Yeongwol组的曲线极为相似。FA3向东南方向增厚,富含页岩的岩层向西北方向盛行,这表明太白山盆地存在地形高低起伏,在沉积早期可能沿着碳酸盐平台形成了斜坡。此外,岩相的相关性和横向厚度变化也表明,盆地在贞善地区西北部的深度较深。盆地变深的原因可能是奥陶纪早期碳酸盐工厂生产力的减弱。
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A new lithostratigraphic scheme of the Ordovician Jeongseon Formation of the Yongtan Group in the Taebaeksan Basin and sequence stratigraphic analysis with discussion on basin geometry

Abstract

Lithostratigraphy of the Yongtan Group is newly established based on detailed sedimentologic and stratigraphic studies on recently exposed, less deformed, relatively continuous outcrops and comprehensive review of previous studies, mainly focusing on the Jeongseon Formation which occupies most of the group spatially and stratigraphically. The Yongtan Group is divided into the Jeongseon, Haengmae, and Hoedongri formations in ascending order, and all the units are assigned to the Ordovician. The Jeongseon Formation is divided into three members based on lithology. Eleven sedimentary facies are recognized in the Jeongseon Formation and organized into five facies associations (FAs), FA1 (tidal flat), FA2 (inner-ramp), FA3 (shoal), FA4 (mid-ramp), and FA5 (ramp-slope to outer-ramp). The formation is interpreted to have been deposited on a homoclinal ramp. The Yongtan Group is divided into two supersequences separated by type 1 sequence boundary and the lower and middle members of the Jeongseon Formation belong to Supersequence I and the Upper Member to Supersequence II which includes the Haengmae and Hoedongri formations. The relative sea-level curve inferred from sequence stratigraphic analysis suggests that the formation evolved through two depositional stages in accordance with second-order sea-level changes separated by the boundary between the Sauk and Tippecanoe sequence, and the curve is greatly similar to that of the Taebaek and Yeongwol groups. The southeastward thickening of FA3 and northwestward prevalence of shale-rich facies suggest that topographic highs and lows were present in the Taebaeksan Basin and a slope might have developed along the carbonate platform during the early stage of deposition. The correlation and lateral thickness variation of the facies associations additionally suggest that the basin was deeper toward the northwestern part of the Jeongseon area. The deepening is likely attributed to the weakening of the productivity of the carbonate factory during the early Ordovician.

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来源期刊
Geosciences Journal
Geosciences Journal 地学-地球科学综合
CiteScore
2.70
自引率
8.30%
发文量
33
审稿时长
6 months
期刊介绍: Geosciences Journal opens a new era for the publication of geoscientific research articles in English, covering geology, geophysics, geochemistry, paleontology, structural geology, mineralogy, petrology, stratigraphy, sedimentology, environmental geology, economic geology, petroleum geology, hydrogeology, remote sensing and planetary geology.
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