碳酸盐岩成岩作用:约翰·安东尼·道森(托尼)·迪克森的工作庆典

IF 1.9 3区地球科学 Q1 GEOLOGY Depositional Record Pub Date : 2023-04-24 DOI:10.1002/dep2.226

V. P. Wright, A. Saller, R. Wood

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引用次数: 0

摘要

对碳酸盐岩的现代认识始于20世纪60年代初，是由许多工人的开创性研究创造的，约翰·安东尼·道森(托尼)·迪克森在这场革命中发挥了重要作用。他的遗产使人们更好地认识到，碳酸盐岩的晶体学、矿物学和地球化学记录了地质时期环境、生物和水文地质过程的复杂相互作用。因此，现在通常会分析碳酸盐岩的气候、大气、海洋学和进化信号，以及描述孔隙度和资源潜力。现代热带碳酸盐沉积物一般为文石和高镁方解石，孔隙度高(Enos & Swatsky, 1981)，而古代碳酸盐(中新世及更老)一般为方解石或白云石，孔隙度低得多。因此，构成碳酸盐岩成岩作用的众多过程是大多数碳酸盐岩历史的基础。破译原始信号，并将其与成岩信号区分开来，需要法医水平的微观研究，这些技术已经由托尼·迪克森(Tony Dickson)开发并不懈地推广。现在，正如本期的论文所说明的那样，我们可以在这个武器库中增加建模和更复杂的地球化学代理的使用。这期《沉积记录》特刊聚焦于对碳酸盐岩成岩作用的细致和创造性的研究，以纪念托尼。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Carbonate diagenesis: A celebration of the work of John Anthony Dawson (Tony) Dickson

Magnesian Limestone zoned dolomite (red and non-luminescent zones) now partly dedolomitized), calcite (yellow luminescence), blue luminescent albite has non-luminescent overgrowths) Mansfield Quarry, Nottinghamshire. Photo credit: J.A.D. Dickson.

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