质量迁移复合体迁移的机制和控制因素:新西兰塔拉纳基深水盆地物质迁移复合体案例研究

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Geomorphology Pub Date : 2024-10-21 DOI:10.1016/j.geomorph.2024.109464
Yongsheng Zhou , Wei Wu , Jianwei Feng , Guangxu Wang , Aihua Fu , Shiqin Liang , Lulu Wu , Qingchao Li , Weiqing Liu , Zhendong Feng , Changsong Lin , Panpan Chen , Jing Yu
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引用次数: 0

摘要

质量输运复合体(MTCs)是大陆坡上重要的沉积物堆积,对自然灾害预测和近海石油勘探具有重要意义。本文利用高清三维地震数据重建了 MTC 的地震地貌和沉积动力学,细致地探索了新西兰 Tanaraki 盆地的沉积系统。它通过运动学符号解译了地震面,量化了巨岩形态特征,并将基底斜坡和河道结构的发展与 MTC 的迁移或运动学结合起来。巨型断块岩有五种地震面类别和动力特征--压缩脊、推力断层、滑坡、沟槽和斜坡阶地。根据属性图和地貌解释,将 MTCs 划分为四个区,显示出剥离、基底斜坡和巨块群对其迁移的综合影响。这些地貌沿线的岩性和地形变化改变了侵蚀特性和 MTCs 的移动性,基底高度的变化引导着局部的迁移轨迹。1 号区和 3 号区的巨岩参数结果调整了我们对应力模式和方向性变化的理解,凸显了复杂的动态变化。值得注意的是,堤坝引发的差异运动造成了纵向剪切带。在临界迁移差异处,MTC 会在这些薄弱点断裂,释放孔隙压力并用细粒填充裂缝,从而形成以低振幅填充为特征的 "海角 "地层。因此,这项研究建立了一个开创性的迁移模型,综合了堤坝高度、岩石类型变化和巨岩堆积强度的影响,描绘了一种支离破碎的迁移模式。这项研究不仅丰富了我们对深水环境中 MTC 行为的掌握,还为衡量 MTC 可能对水下结构造成的危害提供了坚实的科学基础和预测工具,因此具有重要的理论和应用意义。
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Mechanism and controlling factors of mass transport complexes migration: A case study of the mass transport complexes in the taranaki deep water basin, New Zealand
Mass transport Complexes (MTCs) form significant sediment accumulations in continental slopes, hold key insights for natural hazard prediction and offshore oil exploration. This paper uses high-definition 3D seismic data to reconstruct the seismic geomorphology and sedimentary dynamics of MTCs, meticulously exploring the depositional systems of the Tanaraki Basin, New Zealand. It deciphers by kinematic notation, seismic faciess, quantifies megaclast morphological characteristics, in conjunction with the basal slope and channel structure development as the migration or kinematics of MTCs. Five seismic facies categories and dynamic traits—compression ridges, thrust faults, slides, grooves and slope terraces are distinguished in MTCs. Based on attributes maps and geomorphological interpretations, MTCs is segmented into four zones, showing combined effects of levée, basal slopes, and megaclast clusters on its migration. Lithological and topographical variations along these features modulate erosion properties and MTCs mobility, with base height shifts guiding local migration trajectories. The results of megaclast parameters in Zones 1 and 3 tune our understanding of stress patterns and directionality shifts, highlighting the complex dynamics at play. Notably, the differential motion triggered by levees instigates longitudinal shear zones. At critical migration disparities, MTCs fracture at these weak points, discharging pore pressure and filling fractures with fines, birthing “promontory” formations marked by low-amplitude fills. This work, therefore, establishes a groundbreaking migratory model that synthesizes the impacts of levees height, rock type variability, and megaclasts accumulation intensity, depicting a fragmented migration pattern. This study not only enriches our grasp of MTCs behavior in deep-water contexts but also furnishes a robust scientific foundation and predictive tool for gauging the hazards that MTCs may pose to underwater structures, thus carrying substantial theoretical and applied significance.
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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