(Fe–Ca–Al)-Phosphate Mineralization Enriched with Rare Earth Elements in Sediments of the Middle Jurassic Paleovalley (Shankinka Ore Occurrence, Moscow Region, Central Part of the Russian Plate)

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
I. A. Novikov, A. A. Razumovskiy, Yu. V. Yashunskiy, A. A. Alexandrov, E. A. Molkova, P. P. Fedorov
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引用次数: 0

Abstract

A new occurrence of phosphate mineralization (Shankinka) has been explored in the Fedkovskaya River mouth, Ruza district, Moscow region. The most common mineral phases are delvauxite, mitridatite, fluorapatite, and crandallite. The Fe–Ca–Al phosphate occurrences in the region are associated with the Bajocian–Bathonian paleovalleys embedded in Carboniferous rocks and partially filled with Callovian sediments. The structural features of the phosphatization zone along with its enrichment with Co, Ni, Zn, Cu, and REE indicate a possible link between the overlying Oxfordian sediments and phosphate mineralization. The epigenetic phosphate mineralization can be related to the seepage of phosphorus-rich interstitial waters released from the Oxfordian organic-rich sediments into the underlying Callovian friable rocks enriched with Fe minerals.

Abstract Image

(中侏罗世古山谷沉积物中富含稀土元素的(Fe-Ca-Al)-磷酸盐成矿作用(俄罗斯板块中部莫斯科地区香金卡矿点)
摘要 在莫斯科州鲁扎区费德科夫斯卡娅河口勘探到了一个新的磷酸盐矿化点(Shankinka)。最常见的矿物相为白云石、斜长石、氟磷灰石和白云石。该地区的铁-钙-铝磷酸盐矿点与嵌入石炭纪岩石、部分被卡勒维纪沉积物填满的巴约卡-巴托纳古河谷有关。磷化带的结构特征及其富含的钴、镍、锌、铜和稀土元素表明,上覆牛津系沉积物与磷酸盐矿化之间可能存在联系。表生磷酸盐矿化可能与牛背纪富含有机质的沉积物释放出的富磷间隙水渗入下伏富含铁矿物的卡洛维易碎岩有关。
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来源期刊
Lithology and Mineral Resources
Lithology and Mineral Resources 地学-地球化学与地球物理
CiteScore
1.30
自引率
37.50%
发文量
29
审稿时长
>12 weeks
期刊介绍: Lithology and Mineral Resources is an international peer reviewed journal that publishes articles on a wide range of problems related to the formation of sedimentary rocks and ores. Special attention is given to comparison of ancient sedimentary rock and ore formation with present-day processes. The major part of the journal is devoted to comparative analysis of sedimentary processes on the continents and in oceans, as well as the genetic aspects of the formation of sedimentary and hydrothermal–sedimentary mineral resources. The journal welcomes manuscripts from all countries in the English or Russian language.
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