武夷山覆盖区马坑式铁矿层位及找矿方向

狄永军; 张达; 吴淦国; 闫鹏程; 来守华; 龚勇

doi:10.3799/dqkx.2012.131

Volume 37 Issue 6

Jun. 2012

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Article Navigation > Earth Science > 2012 > 37(6): 1232-1242

DI Yong-jun, ZHANG Da, WU Gan-guo, YAN Peng-cheng, LAI Shou-hua, GONG Yong, 2012. Strata Hosted Makeng Type Iron Deposits and Prospecting Orientation in the Wuyishan Covered Region. Earth Science, 37(6): 1232-1242. doi: 10.3799/dqkx.2012.131

Citation:

DI Yong-jun, ZHANG Da, WU Gan-guo, YAN Peng-cheng, LAI Shou-hua, GONG Yong, 2012. Strata Hosted Makeng Type Iron Deposits and Prospecting Orientation in the Wuyishan Covered Region. Earth Science, 37(6): 1232-1242. doi: 10.3799/dqkx.2012.131

Citation:

DI Yong-jun, ZHANG Da, WU Gan-guo, YAN Peng-cheng, LAI Shou-hua, GONG Yong, 2012. Strata Hosted Makeng Type Iron Deposits and Prospecting Orientation in the Wuyishan Covered Region. Earth Science, 37(6): 1232-1242. doi: 10.3799/dqkx.2012.131

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Strata Hosted Makeng Type Iron Deposits and Prospecting Orientation in the Wuyishan Covered Region

doi: 10.3799/dqkx.2012.131

DI Yong-jun^{1, 2
,},
ZHANG Da^{1, 2},
WU Gan-guo^{1, 2},
YAN Peng-cheng^{1, 2},
LAI Shou-hua^{1, 2},
GONG Yong^{1, 2}

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
School of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2012-07-19
Available Online: 2021-11-09
Publish Date: 2012-06-15

Abstract

Abstract

Makeng type iron deposit is a large deposit in the secondary NE-trending Longzhang basal fracture sag zone of the Late Paleozoic depression of Yongmei. The prospecting breakthrough has been hindered due to the fact that we are not very clear about the type of the strata hosted Makeng type iron deposits. On the basis of field investigation and conscientious study of the results of previous researches, this paper explores ore-controlling factors of the Makeng type iron deposit. It is found that the fold in the Makeng mine district is an overturned anticline instead of one limb of the anticline, and that the Yanshanian thrust nappe structure is the results generated by the subduction of Izanagi plate under the Eurasian plate from southeast to northwest. It is suggested that the Jingshe Formation-Qixia Formation (C₂j-P₁q) and interface between the Jingshe Formation-Qixia Formation (C₂j-P₁q) and the Wenbishan Formation (P₁w) are the horizon hosted Makeng type iron deposit, and that the thrust nappe structure is also important ore-controlling factors. In addition, this paper also presents the prospecting direction.
- Makeng type iron deposit,
- overturned anticline,
- nappe structure,
- Wenbishan Formation,
- ore-controlling factor,
- petrology,
- ore prospecting,
- ore deposits

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References(53)

References

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Strata Hosted Makeng Type Iron Deposits and Prospecting Orientation in the Wuyishan Covered Region

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