Genesis of the world’s largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over ~1 b.y.

Song Wenlei, Xu Cheng, Martin Smith, Anton R. Chakhmouradian, Marco Brenna, Jindrich Kynicky, Wei Chen, Yueheng Yang, Miao Deng, Haiyan Tang

Research output: Contribution to journalArticle

Abstract

The unique, giant, rare earth element (REE) deposit at Bayan Obo, northern China, is the world’s largest REE deposit. It is geologically complex, and its genesis is still debated. Here, we report in situ Th-Pb dating and Nd isotope ratios for monazite and Sr isotope ratios for dolomite and apatite from fresh drill cores. The measured monazite ages (361–913 Ma) and previously reported whole-rock Sm-Nd data show a linear relationship with the initial Nd isotope ratio, suggesting a single-stage evolution from a Sm-Nd source that was formed before 913 Ma. All monazites show consistent to those of the adjacent 1.3 Ga carbonatite and mafic dikes. The primary dolomite and apatite show lower than the recrystallized dolomite (0.7038–0.7097). The REE ores at Bayan Obo are interpreted to have originally formed as products of ca. 1.3 Ga carbonatitic magmatism and to have undergone subsequent thermal perturbations induced by Sr-rich, but REE-poor, metamorphic fluids derived from nearby sedimentary rocks.εNd(1.3Ga) values (0.3 ± 0.6) close87Sr/86Sr ratios (0.7024–0.7030)
Original languageEnglish
Pages (from-to)323-326
JournalGeology
Volume46
Issue number4
DOIs
Publication statusPublished - 9 Feb 2018

Fingerprint

rare earth element
mineralization
dolomite
monazite
isotope
apatite
carbonatite
dike
magmatism
sedimentary rock
perturbation
fluid
world
rock

Cite this

Wenlei, Song ; Cheng, Xu ; Smith, Martin ; Chakhmouradian, Anton R. ; Brenna, Marco ; Kynicky, Jindrich ; Chen, Wei ; Yang, Yueheng ; Deng, Miao ; Tang, Haiyan. / Genesis of the world’s largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over ~1 b.y. In: Geology. 2018 ; Vol. 46, No. 4. pp. 323-326.
@article{2e7f6e3e98ae4c4a8e3647b6120c776f,
title = "Genesis of the world’s largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over ~1 b.y.",
abstract = "The unique, giant, rare earth element (REE) deposit at Bayan Obo, northern China, is the world’s largest REE deposit. It is geologically complex, and its genesis is still debated. Here, we report in situ Th-Pb dating and Nd isotope ratios for monazite and Sr isotope ratios for dolomite and apatite from fresh drill cores. The measured monazite ages (361–913 Ma) and previously reported whole-rock Sm-Nd data show a linear relationship with the initial Nd isotope ratio, suggesting a single-stage evolution from a Sm-Nd source that was formed before 913 Ma. All monazites show consistent to those of the adjacent 1.3 Ga carbonatite and mafic dikes. The primary dolomite and apatite show lower than the recrystallized dolomite (0.7038–0.7097). The REE ores at Bayan Obo are interpreted to have originally formed as products of ca. 1.3 Ga carbonatitic magmatism and to have undergone subsequent thermal perturbations induced by Sr-rich, but REE-poor, metamorphic fluids derived from nearby sedimentary rocks.εNd(1.3Ga) values (0.3 ± 0.6) close87Sr/86Sr ratios (0.7024–0.7030)",
author = "Song Wenlei and Xu Cheng and Martin Smith and Chakhmouradian, {Anton R.} and Marco Brenna and Jindrich Kynicky and Wei Chen and Yueheng Yang and Miao Deng and Haiyan Tang",
year = "2018",
month = "2",
day = "9",
doi = "10.1130/G39801.1",
language = "English",
volume = "46",
pages = "323--326",
journal = "Geology",
issn = "0091-7613",
number = "4",

}

Wenlei, S, Cheng, X, Smith, M, Chakhmouradian, AR, Brenna, M, Kynicky, J, Chen, W, Yang, Y, Deng, M & Tang, H 2018, 'Genesis of the world’s largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over ~1 b.y.', Geology, vol. 46, no. 4, pp. 323-326. https://doi.org/10.1130/G39801.1

Genesis of the world’s largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over ~1 b.y. / Wenlei, Song; Cheng, Xu; Smith, Martin; Chakhmouradian, Anton R.; Brenna, Marco; Kynicky, Jindrich; Chen, Wei; Yang, Yueheng; Deng, Miao; Tang, Haiyan.

In: Geology, Vol. 46, No. 4, 09.02.2018, p. 323-326.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Genesis of the world’s largest rare earth element deposit, Bayan Obo, China: Protracted mineralization evolution over ~1 b.y.

AU - Wenlei, Song

AU - Cheng, Xu

AU - Smith, Martin

AU - Chakhmouradian, Anton R.

AU - Brenna, Marco

AU - Kynicky, Jindrich

AU - Chen, Wei

AU - Yang, Yueheng

AU - Deng, Miao

AU - Tang, Haiyan

PY - 2018/2/9

Y1 - 2018/2/9

N2 - The unique, giant, rare earth element (REE) deposit at Bayan Obo, northern China, is the world’s largest REE deposit. It is geologically complex, and its genesis is still debated. Here, we report in situ Th-Pb dating and Nd isotope ratios for monazite and Sr isotope ratios for dolomite and apatite from fresh drill cores. The measured monazite ages (361–913 Ma) and previously reported whole-rock Sm-Nd data show a linear relationship with the initial Nd isotope ratio, suggesting a single-stage evolution from a Sm-Nd source that was formed before 913 Ma. All monazites show consistent to those of the adjacent 1.3 Ga carbonatite and mafic dikes. The primary dolomite and apatite show lower than the recrystallized dolomite (0.7038–0.7097). The REE ores at Bayan Obo are interpreted to have originally formed as products of ca. 1.3 Ga carbonatitic magmatism and to have undergone subsequent thermal perturbations induced by Sr-rich, but REE-poor, metamorphic fluids derived from nearby sedimentary rocks.εNd(1.3Ga) values (0.3 ± 0.6) close87Sr/86Sr ratios (0.7024–0.7030)

AB - The unique, giant, rare earth element (REE) deposit at Bayan Obo, northern China, is the world’s largest REE deposit. It is geologically complex, and its genesis is still debated. Here, we report in situ Th-Pb dating and Nd isotope ratios for monazite and Sr isotope ratios for dolomite and apatite from fresh drill cores. The measured monazite ages (361–913 Ma) and previously reported whole-rock Sm-Nd data show a linear relationship with the initial Nd isotope ratio, suggesting a single-stage evolution from a Sm-Nd source that was formed before 913 Ma. All monazites show consistent to those of the adjacent 1.3 Ga carbonatite and mafic dikes. The primary dolomite and apatite show lower than the recrystallized dolomite (0.7038–0.7097). The REE ores at Bayan Obo are interpreted to have originally formed as products of ca. 1.3 Ga carbonatitic magmatism and to have undergone subsequent thermal perturbations induced by Sr-rich, but REE-poor, metamorphic fluids derived from nearby sedimentary rocks.εNd(1.3Ga) values (0.3 ± 0.6) close87Sr/86Sr ratios (0.7024–0.7030)

U2 - 10.1130/G39801.1

DO - 10.1130/G39801.1

M3 - Article

VL - 46

SP - 323

EP - 326

JO - Geology

JF - Geology

SN - 0091-7613

IS - 4

ER -