METALLOGENIC STRUCTCTURAL PLANE CHARACTERISTICS AND ITS PROSPECTING IMPORTANCE FOR THE MAKENG TYPE IRON DEPOSITS IN SOUTHWESTERN FUJIAN PROVINCE

WANG Sen; ZHANG Da; WU Ganguo; YI Jinjun; LI Xingjian; YU Tengda; BAI Yu; GAO Xiaoqiao

doi:10.12090/j.issn.1006-6616.2018.24.02.021

Volume 24 Issue 2

Apr. 2018

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WANG Sen, ZHANG Da, WU Ganguo, et al., 2018. METALLOGENIC STRUCTCTURAL PLANE CHARACTERISTICS AND ITS PROSPECTING IMPORTANCE FOR THE MAKENG TYPE IRON DEPOSITS IN SOUTHWESTERN FUJIAN PROVINCE. Journal of Geomechanics, 24 (2): 199-211. DOI: 10.12090/j.issn.1006-6616.2018.24.02.021

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METALLOGENIC STRUCTCTURAL PLANE CHARACTERISTICS AND ITS PROSPECTING IMPORTANCE FOR THE MAKENG TYPE IRON DEPOSITS IN SOUTHWESTERN FUJIAN PROVINCE

doi: 10.12090/j.issn.1006-6616.2018.24.02.021

WANG Sen^{1, 2, 3
,},
ZHANG Da^{1
,
,},
WU Ganguo¹,
YI Jinjun¹,
LI Xingjian¹,
YU Tengda¹,
BAI Yu¹,
GAO Xiaoqiao¹

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
Beijing Institute of Exploration Engineering, China Geological Survey, Beijing 100083, China
3.
Inner Mongolia Mining Development Limited Liability Company, Hohhot 010010, Inner Mongolia, China

More Information

Received: 2017-07-28
Revised: 2018-02-27
Published: 2018-04-01

Abstract

Abstract

Located in the Late Paleozoic depression of southwestern Fujian, the Makeng type iron deposits are the main skarn iron polymetallic deposits. The major ore bodies are generally controlled by lithologic boundaries and tectonic structural planes, especially the interface between silica and calcareous bed, and they are located above the quartz sandstone of the Lower Carboniferous Lindi formation(C₁l)and below the carbonate rocks of the Upper Carboniferous Jingshe formation-Upper Permian Qixia formation(C₂j-P₂q). In order to reveal the genesis and mineralization mechanism of the Makeng type iron deposits, the Si/Ca surface ore-controlling theory was used to discuss the metallogenic structctural plane characteristics and its ore-controlling mechanism. Five types of metallogenic interfaces were divided according to their features in this research. We deemed that the main ore bodies of Makeng type iron deposits were controlled by the physical and chemical differences between these Ca/Si surfaces, and it is easy to form expansion space and geochemical barrier near the surfaces in the process of tectonic and fluidic activities. Based on the understanding above, the metallogenic model of the Makeng type iron deposits was built using the Si/Ca surface ore-controlling theory. This work is thought to be meaningful to conduct prospecting research of iron polymetallic deposits in southwestern Fujian Province.
- Makeng type iron deposit,
- metallogenic structctural plane,
- Si/Ca surface,
- southwestern Fujian

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METALLOGENIC STRUCTCTURAL PLANE CHARACTERISTICS AND ITS PROSPECTING IMPORTANCE FOR THE MAKENG TYPE IRON DEPOSITS IN SOUTHWESTERN FUJIAN PROVINCE

doi: 10.12090/j.issn.1006-6616.2018.24.02.021

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METALLOGENIC STRUCTCTURAL PLANE CHARACTERISTICS AND ITS PROSPECTING IMPORTANCE FOR THE MAKENG TYPE IRON DEPOSITS IN SOUTHWESTERN FUJIAN PROVINCE

doi: 10.12090/j.issn.1006-6616.2018.24.02.021

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