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Using zircon U-Pb ages to constrain the provenance and transport of heavy minerals within the northwestern shelf of the South China Sea

机译:利用锆石U-pb年龄来限制南海西北陆架内重矿物的来源和运输

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摘要

Numerous ore-grade heavy mineral placer deposits occur in the northern South China Sea region. Previous studies on these deposits have focused on the heavy-mineral ore resources themselves, but the provenance and transport pathways of these heavy minerals are poorly constrained. This paper presents U-Pb ages of detrital zircons from sediments within the northwestern shelf of the South China Sea, and uses this new dataset to determine the provenance and transport pathway of the sediments. Zircons in sediments from ten areas of the northwestern shelf exhibit distinct age populations, suggesting that they have multiple provenances. Zircons in sediments from the Pearl River Mouth, Shangchuan Island, and Moyang River Mouth areas all have an obvious peak of Mesozoic ages, indicating that they have similar sediment provenances; i.e., mainly from the Pearl River, and to a lesser degree from the Moyang River. Zircons in sediments from the areas around the Jian River Mouth and Leizhou Bay, and off Hainan Island have an early Paleozoic age, suggesting that the sediments predominantly originate from the Yunkai massif. Zircons of the sediments from the remaining four areas, the Leigiong Strait, Wanquan River Mouth, Qiongdongnan, and the Outer Shelf, have Yanshannian and Indosinian age peaks in addition to an obvious early Paleozoic population, implying mixed provenances, including the Yunkai massif and Hainan Island. The sediment transport may have involved two hydrodynamic conditions in two distinct stages. First, the Guangdong Longshore Current carried the river sediments to where they dispersed in the inner shelf; subsequently, wave-induced strong currents further transported sandy sediments southeastward to the outer shelf. In addition to explaining the provenance and transport pathways of heavy minerals within the northwestern shelf of the South China Sea, these results provide new information relevant to exploration for heavy-mineral placer deposits. (C) 2016 Published by Elsevier Ltd.
机译:南海北部地区有许多矿石级的重矿物砂矿床。以前对这些矿床的研究都集中在重矿物资源本身上,但是这些重矿物的来源和运输途径受到的限制很有限。本文介绍了南海西北陆架内沉积物中碎屑锆石的U-Pb年龄,并使用此新数据集确定了沉积物的来源和运输途径。西北大陆架十个地区的沉积物中的锆石显示出不同的年龄种群,表明它们具有多种出处。珠江口,上川岛和Mo阳河口地区沉积物中的锆石均具有明显的中生代年龄高峰,表明其物源相似。即主要来自珠江,而程度较小的则来自the阳河。剑江口和雷州湾周围以及海南岛以外地区沉积物中的锆石具有早古生代,表明这些沉积物主要来自云开地块。雷公海峡,万泉河口,琼东南和外陆架这四个地区的沉积物锆石除具有明显的早古生代外,还具有燕山年和印支期的年龄高峰,这意味着云凯地块和海南的物源混杂。岛。泥沙输送可能在两个不同的阶段涉及到两个流体动力条件。首先,广东长岸洋流将河道沉积物带到内陆架。随后,波浪引起的强流将砂状沉积物进一步向东南输送到外陆架。这些结果除了解释南海西北部陆架内重矿物的来源和运输途径外,还为重矿物砂矿的勘探提供了新的信息。 (C)2016由Elsevier Ltd.出版

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