Quantifying the Criteria Used to Identify Zircons from Ore-Bearing and Barren Systems in Porphyry Copper Exploration

IF 5.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Economic Geology Pub Date : 2024-07-04 DOI:10.5382/econgeo.5086
Carlos Carrasco-Godoy, Ian H. Campbell, Yamila Cajal
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Abstract

Zircon is a common mineral in igneous rocks, which is resistant to both chemical weathering and physical abrasion. Its chemistry can potentially be used to distinguish ore-forming porphyry magmas from barren magma systems. This study compiles >23,000 zircon analyses from >30 porphyry deposits, barren intrusions, and rivers to determine the principal geochemical characteristics of fertile zircons using predictive modeling, and compares them with traditional geochemical thresholds. The results show that the Eu/Eu* and Dy/Yb ratios, P content, and the curvature at the end of rare earth element (REE) patterns (λ3) are the most diagnostic characteristics of fertile zircons. The use of geochemical thresholds, as Boolean conditions, reach their maximum performance for Eu/Eu* and Dy/Yb (sensitivity [sens] = 0.73, specificity [spec] = 0.90), but it is outperformed by the random forest model (sens = 0.91, spec = 0.93) in the testing set. Explanatory analysis of the models shows that the fertility signal in zircons becomes stronger as the porphyry system evolves and is accompanied by an overall decrease in the middle to light REE and P content, characteristics that are absent in barren zircons. We attribute the observed difference in λ3 to the co-crystallization of other accessory phases, suggesting that the changes in the zircon Ce anomaly is controlled by the depletion of light and middle REE. The low P content in fertile zircons is caused by extensive crystallization of apatite. Fertile zircons have an excess of (REE + Y)3+, which we attribute to charge-balance by H+ in hydrous magmas. Simple machine learning algorithms outperform the traditional geochemical discriminators in their predictions and provide insights into characteristics that have not previously been considered for evaluating porphyry copper fertility using zircon geochemistry. We propose simplified methods that can be easily incorporated into exploration workflows.
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在斑岩铜矿勘探中量化用于识别含矿和贫矿系统锆石的标准
锆石是火成岩中一种常见的矿物,具有抗化学风化和物理磨损的特性。锆石的化学性质可用于区分成矿斑岩岩浆和贫瘠岩浆系统。本研究汇编了来自 30 多个斑岩矿床、贫瘠侵入体和河流的 23,000 多份锆石分析报告,利用预测建模确定了肥沃锆石的主要地球化学特征,并将其与传统的地球化学阈值进行了比较。结果表明,Eu/Eu* 和 Dy/Yb 比率、P 含量以及稀土元素(REE)图案末端的曲率 (λ3) 是可育锆石最具诊断性的特征。使用地球化学阈值作为布尔条件,在 Eu/Eu* 和 Dy/Yb 方面达到了最高性能(灵敏度 [sens] = 0.73,特异度 [spec] = 0.90),但在测试集中,它的性能被随机森林模型(灵敏度 = 0.91,特异度 = 0.93)所超越。对模型的解释性分析表明,随着斑岩系统的演化,锆石中的肥度信号变得更强,同时伴随着中轻度 REE 和 P 含量的整体下降,而这些特征在贫瘠锆石中是不存在的。我们将观测到的λ3差异归因于其他附属相的共晶化,这表明锆石Ce异常的变化是由轻型和中型REE的损耗控制的。可育锆石中的低 P 含量是由磷灰石的大量结晶造成的。肥沃锆石中 (REE + Y)3+ 过量,我们将其归因于含水岩浆中 H+ 的电荷平衡。简单的机器学习算法在预测方面优于传统的地球化学判别器,并对以前在利用锆石地球化学评估斑岩铜富集度时未曾考虑过的特征提出了见解。我们提出的简化方法可轻松纳入勘探工作流程。
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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来源期刊
Economic Geology
Economic Geology 地学-地球化学与地球物理
CiteScore
10.00
自引率
6.90%
发文量
120
审稿时长
6 months
期刊介绍: The journal, now published semi-quarterly, was first published in 1905 by the Economic Geology Publishing Company (PUBCO), a not-for-profit company established for the purpose of publishing a periodical devoted to economic geology. On the founding of SEG in 1920, a cooperative arrangement between PUBCO and SEG made the journal the official organ of the Society, and PUBCO agreed to carry the Society''s name on the front cover under the heading "Bulletin of the Society of Economic Geologists". PUBCO and SEG continued to operate as cooperating but separate entities until 2001, when the Board of Directors of PUBCO and the Council of SEG, by unanimous consent, approved a formal agreement of merger. The former activities of the PUBCO Board of Directors are now carried out by a Publications Board, a new self-governing unit within SEG.
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