海岸到陆架环境的混合沉积过程:朝向承认其复杂性

IF 1.9 3区地球科学 Q1 GEOLOGY

Depositional Record Pub Date : 2023-03-27 DOI:10.1002/dep2.229

Valentin Zuchuat, Marcello Gugliotta, Miquel Poyatos-Moré, Helena van der Vegt, Daniel S. Collins, Romain Vaucher

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引用次数: 0

摘要

混合能沉积过程是指在一定的沉积环境中，控制沉积动力学的水动力过程的相互作用。当提到海岸到大陆架领域时，三种主要的过程被认为是主要的参与者:河流、潮汐和波浪(Ainsworth等人，2011;Dalrymple et al.， 1992;Dashtgard等人，2021;Zuchuat et al.， 2019)。除了这些过程的周期性或准时的内在变化外，风成过程、等高线流、季节性冰盖、基岩的性质和力学特征以及盆地的限制和地貌、气候振荡(例如El Niño和La Niña)和相对海平面波动也可与这三个主要过程相互作用或影响，在沉积分析中也应予以考虑。在现代环境中，沉积过程的定性依赖于直接测量(例如，流速、水位变化、波高、悬浮沉积物浓度、粘土浓度)。然后，定量测量可以与对所得沉积产物(即形态、层状)和生物成因元素(即微量化石)的更定性描述相结合(Dashtgard等人，2009;Vaucher et al.， 2018;Vaucher & Dashtgard, 2022;Yang et al.， 2008;Yang & Chang, 2017)。此外，实验研究有助于从地层中提炼对单个和组合过程的解释，这些解释虽然不能诊断特定的沉积环境，但可以用来重建沉积过程，因此有助于古环境解释(Arnott & Southard, 1990;Baas et al.， 2021;Cummings et al.， 2009;Dumas et al.， 2005;Dumas & Arnott, 2006;Myrow等人，2018;Perillo et al.， 2014;Sato et al.， 2011;Southard等人，1990;Southard & Boguchwal, 1990)。主要端元过程的地层模型和相解释是历史上发展起来的。收稿:2023年2月28日|修订:2023年3月6日|接受:2023年3月23日DOI: 10.1002/dep2.229

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Mixed depositional processes in coastal to shelf environments: Towards acknowledging their complexity

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Mixed depositional processes in coastal to shelf environments: Towards acknowledging their complexity

Sketch diagram illustrating the various hydrodynamic processes occurring in coastal to shelf environments, with numbers referring to articles from this issue.

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来源期刊

Depositional Record GEOLOGY-

CiteScore

4.10

自引率

16.70%

发文量

审稿时长

16 weeks