Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation

The Duobaoshan Cu (Mo) deposit is one of the oldest super large porphyry deposits in the eastern part of the Central Asian orogenic belt. Although ore-forming processes have been extensively concerned, the post-mineralization ore preservation state was poorly focused on. In order to improve the abil...

Full description

Saved in:
Bibliographic Details
Main Authors: Yaxing Leng, Jianping Wang, Dewen Zheng
Format: Article
Language:English
Published: Wiley 2022-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2022/2948701
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1849308405412397056
author Yaxing Leng
Jianping Wang
Dewen Zheng
author_facet Yaxing Leng
Jianping Wang
Dewen Zheng
author_sort Yaxing Leng
collection DOAJ
description The Duobaoshan Cu (Mo) deposit is one of the oldest super large porphyry deposits in the eastern part of the Central Asian orogenic belt. Although ore-forming processes have been extensively concerned, the post-mineralization ore preservation state was poorly focused on. In order to improve the ability of prospecting forecast, it is necessary to consider both deposit formation and deposit preservation. Here, we reported apatite fission track (AFT) data for the Duobaoshan porphyry copper deposits in the belt to reveal the cooling and exhumation history and evaluate ore preservation. The results show that the rapid cooling of the ore-hosting rock body occurred later than the surrounding rock body. The rapid cooling of the surrounding granodiorite occurred between 82 and 72 Ma, with the exhumation depth of 2.33–3.11 km and the exhumation rate of 0.25 mm/a, whereas the ore-hosting granodiorite porphyry was rapid cooling between 71.8 and 50.2 Ma, with the exhumation depth of 2.99–3.86 km and the exhumation rate of 0.22 mm/a. This differential exhumation and cooling event provide favorable geological conditions for the preservation of the ore body.
format Article
id doaj-art-059b1712b5eb46688b121554b9c851a0
institution Kabale University
issn 1468-8123
language English
publishDate 2022-01-01
publisher Wiley
record_format Article
series Geofluids
spelling doaj-art-059b1712b5eb46688b121554b9c851a02025-08-20T03:54:28ZengWileyGeofluids1468-81232022-01-01202210.1155/2022/2948701Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore PreservationYaxing Leng0Jianping Wang1Dewen Zheng2Chinese Academy of Geological SciencesChina University of Geosciences (Beijing)Guangzhou Institute of GeochemistryThe Duobaoshan Cu (Mo) deposit is one of the oldest super large porphyry deposits in the eastern part of the Central Asian orogenic belt. Although ore-forming processes have been extensively concerned, the post-mineralization ore preservation state was poorly focused on. In order to improve the ability of prospecting forecast, it is necessary to consider both deposit formation and deposit preservation. Here, we reported apatite fission track (AFT) data for the Duobaoshan porphyry copper deposits in the belt to reveal the cooling and exhumation history and evaluate ore preservation. The results show that the rapid cooling of the ore-hosting rock body occurred later than the surrounding rock body. The rapid cooling of the surrounding granodiorite occurred between 82 and 72 Ma, with the exhumation depth of 2.33–3.11 km and the exhumation rate of 0.25 mm/a, whereas the ore-hosting granodiorite porphyry was rapid cooling between 71.8 and 50.2 Ma, with the exhumation depth of 2.99–3.86 km and the exhumation rate of 0.22 mm/a. This differential exhumation and cooling event provide favorable geological conditions for the preservation of the ore body.http://dx.doi.org/10.1155/2022/2948701
spellingShingle Yaxing Leng
Jianping Wang
Dewen Zheng
Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation
Geofluids
title Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation
title_full Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation
title_fullStr Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation
title_full_unstemmed Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation
title_short Apatite Fission Track Thermochronology of Granite from Duobaoshan Porphyry Cu (Mo) Deposit, Northeast China: Implications for Cooling History and Ore Preservation
title_sort apatite fission track thermochronology of granite from duobaoshan porphyry cu mo deposit northeast china implications for cooling history and ore preservation
url http://dx.doi.org/10.1155/2022/2948701
work_keys_str_mv AT yaxingleng apatitefissiontrackthermochronologyofgranitefromduobaoshanporphyrycumodepositnortheastchinaimplicationsforcoolinghistoryandorepreservation
AT jianpingwang apatitefissiontrackthermochronologyofgranitefromduobaoshanporphyrycumodepositnortheastchinaimplicationsforcoolinghistoryandorepreservation
AT dewenzheng apatitefissiontrackthermochronologyofgranitefromduobaoshanporphyrycumodepositnortheastchinaimplicationsforcoolinghistoryandorepreservation