墨西哥湾西部海岸沙丘砂中辉石质碎屑的表面结构:对其保存和地球环境过程的影响

IF 1.9 3区 地球科学 Q1 GEOLOGY Depositional Record Pub Date : 2023-04-25 DOI:10.1002/dep2.228
Juan J. Kasper-Zubillaga, Raymundo Gerardo Martínez-Serrano, David M. Buchs, Mauricio Mendieta-Lora, Elsa Arellano-Torres, León Felipe Álvarez-Sánchez
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摘要

本文研究辉石颗粒的表面结构和形态在其源-汇历史中是如何演变的。本研究适用于墨西哥湾海岸沙丘砂中的斜辉石碎屑,这些碎屑来源于跨墨西哥火山带,然后在受有限化学风化作用的环境中运输和沉积。利用单粒地球化学分析和表面纹理图像对辉石的组成和形态进行了表征,并采用基于致密性的新方法来评估矿物的形状。这揭示了非均质透辉岩种群,其矿物形态主要受沿解理的冲击破碎控制,边缘的物理磨损很少,化学风化的证据有限。机械表面纹理优于机械/化学和化学表面纹理。这些机械表面结构主要保存为平坦的理裂面和圆形的边缘,分别继承自河流-潮间带和风成搬运。机械/化学诱导的表面纹理被保存为细长的凹陷。化学表面结构稀疏,主要以乳状结构为代表,表明在水下条件下局部溶解。化学表面结构的稀缺性是由于斜辉石常沿解理破碎,以及在观察到的种群运输过程中化学风化作用有限。海岸沙丘砂中的斜辉石颗粒主要保留了河流搬运的表面特征。尽管沿着解理的矿物破碎可能会在风化有限的侵蚀机制下模糊它们的原始形态,但这项研究表明,辉石颗粒的表面结构和形态如何用于确定火山环境附近的运输和沉积事件。使用致密性作为粒子的形状描述子测量提供了另一种方法来观察尽管沿海地区的高能量条件下斜辉石如何保持不变。
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Surface textures of detrital pyroxenes in coastal dune sands (western Gulf of Mexico, Mexico): Implications for their preservation and geoenvironmental processes

This work investigates how the surface textures and morphology of pyroxene grains evolve during their source-to-sink history. This study applies to detrital clinopyroxenes concentrated in coastal dune sands of the Gulf of Mexico which were sourced in the Trans Mexican Volcanic Belt then transported and deposited in environments subject to limited chemical weathering. The composition and morphology of the pyroxenes was characterised using single-grain geochemical analysis and surface texture imagery with a novel approach based on the compactness property to assess the shape of minerals. This reveals heterogenous diopside-augite populations, displaying mineral morphologies dominantly controlled by impact breakage along cleavages, little physical abrasion along their edges and with limited evidence for chemical weathering. Mechanical surface textures dominate over mechanical/chemical and chemical surface textures. These mechanical surface textures are preserved primarily as flat cleavage surfaces and rounded edges inherited from fluvial-intertidal and aeolian transport, respectively. Mechanically/chemically induced surface textures are preserved as elongated depressions. Chemical surface textures are sparse and mostly represented by mammillated textures that suggest local dissolution under subaqueous conditions. The scarcity of chemical surface textures is attributed to frequent fragmentation of the clinopyroxenes along cleavages and limited chemical weathering during transport of the observed populations. Clinopyroxene grains in the coastal dune sands primarily retain surface characteristics from fluvial transport. Although the breakage of minerals along cleavages can obscure their original morphology under a weathering-limited erosion regime, this study shows how surface textures and morphology of pyroxene grains is used to determine episodes of transport and deposition close to volcanic environments. The use of the compactness property as a shape descriptor measurement of particles provides an alternative approach to observe how clinopyroxene remains unaltered despite the high energy conditions of the coastal area.

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来源期刊
CiteScore
4.10
自引率
16.70%
发文量
42
审稿时长
16 weeks
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