Mineralization and magmatic origin of the 2.1 Ga Zhaoanzhuang magnetite-apatite deposit, North China Craton: Constraints on the formation of the Paleoproterozoic iron oxide-apatite deposits

Iron oxide-apatite (IOA) deposits provide large amounts of iron for steel industry worldwide, but their origins are still in dispute. Although IOA deposits were commonly genetically related to intermediate-mafic igneous rocks, the occurrences of IOA deposits in ultramafic rocks are scarce. The Zhaoa...

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Bibliographic Details
Published in:Precambrian Research
Main Authors: Lan, Caiyun, Long, Xiaoping, Zhao, Taiping, Zhai, Mingguo
Format: Report
Language:English
Published: ELSEVIER 2022
Subjects:
Geology
Iron oxide-apatite
Magnetite
Apatite
Fe -O isotope
In-situ Sr-Nd isotope
Zhaoanzhuang
Geosciences
Multidisciplinary
HYDROTHERMAL PROCESSES EVIDENCE
TRACE-ELEMENT CONCENTRATIONS
KIRUNA-TYPE
OXYGEN-ISOTOPE
CARBONATITE COMPLEX
ACCESSORY MINERALS
SOUTHEAST MISSOURI
PEA RIDGE
GEOCHEMISTRY
MANTLE
Kiruna
Online Access:http://ir.gig.ac.cn/handle/344008/68461
https://doi.org/10.1016/j.precamres.2022.106839
Description
Summary:Iron oxide-apatite (IOA) deposits provide large amounts of iron for steel industry worldwide, but their origins are still in dispute. Although IOA deposits were commonly genetically related to intermediate-mafic igneous rocks, the occurrences of IOA deposits in ultramafic rocks are scarce. The Zhaoanzhuang iron deposit in the North China Craton is characterized by comprising abundant low-Ti magnetite, apatite and ultramafic minerals (e.g., olivine, orthopyroxene), but its origin has long been controversial. These ultramafic minerals mainly occur as aggregates surrounded by magnetite in the iron ores and display typical cumulate textures and high Fo values, indicative of magmatic origin. The delta 56Fe and delta 18O values of magnetite from the ores range from 0.22 & PLUSMN; 0.03%o to 0.32 & PLUSMN; 0.03%o and from 2.6%o to 4.5%o, respectively, akin to those in magmatic rocks and IOA deposits but distinct from those of metamorphic BIFs. Both types of apatite occurring in the ultramafic aggregates and the iron ores contain 2.07 to 2.69 wt% F, less than 0.65 wt% Cl, up to 7900 ppm rare earth elements (REE) and greatly variable Sr-Nd isotopic compositions, reflecting that both types are of magmatic-hydrothermal origin. The crust-like epsilon Nd(t) values (-7.1 to-5.2) of all apatite grains record reset of their Sm-Nd system, which is resulted from the involvement of carbonate fluids based on their similar REE patterns. In situ Sm-Nd isotope analyses of apatite from the ultramafic aggregates and the iron ores have yielded similar Sm-Nd isochron ages at 2100 & PLUSMN; 81 Ma (MSWD = 0.84) and 2096 & PLUSMN; 240 Ma (MSWD = 0.85), respectively, which can constrain the minimum age for the Fe mineralization. Combined with sedimentary age of the strata, the ore-forming age of the deposit was 2.3-2.1 Ga. The negative epsilon Nd(t) values of the ultramafic aggregates (-1.2 to-1.0), the iron ores (-1.8 to-1.5) and magnetite (-1.6 to-0.8) from the ores indicate that the ore-forming magma has a slightly enriched ...

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