The Relationship between Sequence Stratigraphy and Groundwater of Quaternary Sediments in Relation to Global Sea-level Change in the Downstream Red River Delta Area

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Lithology and Mineral Resources Pub Date : 2022-09-12 DOI:10.1134/S002449022205008X
Tran Nghi, Do Tien Hung, Trinh Hoai Thu, Renat Shakirov, Nadezhda Syrbu, Ngo Quang Toan, Hoang Anh Khien, Tran Thi Thuy Huong, Natalia Lee, Dinh Xuan Thanh, Tran Thi Thanh Nhan, Nguyen Thi Huyen Trang, Nguyen Thi Phuong Thao, Tran Thi Dung, Tran Ngoc Dien
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Abstract

The study of the distribution law and origin of groundwater in Quaternary sediments downstream of the Red River Delta is approached in the direction of research on sequence stratigraphy and the distribution law of lithofacies according to space and time. However, the distribution law of lithofacies and groundwater depends on global sea-level changes and tectonic activities as the two most important reasons. Quaternary sediments of the Red River delta downstream have 5 sediment cycles corresponding to 5 sequences: (1) sequence 1 with Early Pleistocene age (Sq1\({\text{Q}}_{1}^{1}\)); (2) sequence 2 with early Middle Pleistocene age (Sq2\({\text{Q}}_{1}^{{2{\text{a}}}}\)); (3) sequence 3 with late middle Pleistocene age (Sq3\({\text{Q}}_{1}^{{2{\text{b}}}}\)); (4) sequence 4 with early Pleistocene age (Sq4\({\text{Q}}_{1}^{{3{\text{a}}}}\)); (5) sequence 5 with late Pleistocene–Holocene age (Sq5\({\text{Q}}_{1}^{{3{\text{b}}}}\)–Q2). Each sequence is composed of three sedimentary systems tracts. The lowstand systems tract (LST) is characterized by a lowstand alluvial muddy sand facies complex that acts as a primary freshwater aquifer (SmarLST). The transgressive systems tract (TST) is characterized by a coastal swamp sand mud facies (MsamtTST) and a maximum transgression bay-lagoon mud facies (MmtTST) acting as an aquifuge. The highstand systems tract (HST) is characterized by sand bar facies (SamhHST) and delta plain sandy mud facies (MsamhHST). Thus, vertically Pleistocene sediments have 5 aquifers, in which each aquifer is constituted by the superposition of two successive facies complex: (1) upper part: lowstand alluvial gravelly sand facies complex (LST) and (2) lower part: highstand dune sand bar facies complex (SarLST/SamhHST). The spatial distribution of freshwater aquifers in 3 provinces Northwest Thai Binh, Ninh Binh—southeast Nam Dinh, and northwest Nam Dinh demonstrate the absence of shallow marine-bay mud facies.

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红河三角洲下游地区第四纪沉积物层序地层与地下水与全球海平面变化的关系
从层序地层学和岩相时空分布规律的研究方向,探讨了红河三角洲下游第四纪沉积物中地下水的分布规律和成因。然而,岩相和地下水的分布规律取决于全球海平面变化和构造活动是两个最重要的原因。红河三角洲下游第四纪沉积物有5个沉积旋回,对应5个层序:(1)层序1为早更新世(Sq1 - \({\text{Q}}_{1}^{1}\));(2)中更新世早期层序2 (Sq2 - \({\text{Q}}_{1}^{{2{\text{a}}}}\));(3)层序3代表中更新世晚期(Sq3 - \({\text{Q}}_{1}^{{2{\text{b}}}}\));(4)层序4为早更新世时代(Sq4 - \({\text{Q}}_{1}^{{3{\text{a}}}}\));(5)序列5代表晚更新世-全新世时代(Sq5 - \({\text{Q}}_{1}^{{3{\text{b}}}}\) - q2)。每个层序由三个沉积体系域组成。低水位体系域(LST)以低水位冲积泥砂相复合体为特征,作为初级淡水含水层(SmarLST)。海侵体系域(TST)以滨海沼泽砂泥相(MsamtTST)和最大海侵海湾-泻湖泥相(MmtTST)为特征。高地体系域以沙坝相(SamhHST)和三角洲平原砂泥相(MsamhHST)为特征。因此,垂直更新世沉积物有5个含水层,每个含水层由两个连续相复合体叠加而成:(1)上部为低水位冲积砾石砂相复合体(LST),(2)下部为高水位沙丘沙坝相复合体(SarLST/SamhHST)。泰平西北部、宁平-南定东南部和南定西北部3个省的淡水含水层空间分布表明不存在浅海-海湾泥相。
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来源期刊
Lithology and Mineral Resources
Lithology and Mineral Resources 地学-地球化学与地球物理
CiteScore
1.30
自引率
37.50%
发文量
29
审稿时长
>12 weeks
期刊介绍: Lithology and Mineral Resources is an international peer reviewed journal that publishes articles on a wide range of problems related to the formation of sedimentary rocks and ores. Special attention is given to comparison of ancient sedimentary rock and ore formation with present-day processes. The major part of the journal is devoted to comparative analysis of sedimentary processes on the continents and in oceans, as well as the genetic aspects of the formation of sedimentary and hydrothermal–sedimentary mineral resources. The journal welcomes manuscripts from all countries in the English or Russian language.
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