Sains
Malaysiana 46(11)(2017): 2149-2162
http://dx.doi.org/10.17576/jsm-2017-4611-16
Non-seismic
Geophysical Prospecting Model of Beiya Gold Mine in Western
Yunnan Province
(Model
Pencarigalian Geofizik tak Seismik Lombong Emas Beiya di Wilayah
Barat Yunnan)
JIAN
YANG1*, QIAO WANG1, SHENGXIAN LIANG1,
JING GUO1 & MUHAMMAD
AQEEL
ASHRAF2
1Chengdu Center, China Geological
Survey, Chengdu 610081, China
2International Water, Air & Soil
Conservation Society, 59200 Kuala Lumpur, Federal Territory
Malaysia
Received:
25 January 2017/Accepted: 25 May 2017
ABSTRACT
According to the basic rules and characteristics of the gold-polymetallic
deposits of Beiya gold mine area in terms of mineralization
and ore controlling, it is concluded that skarn deposit is the
main ore deposit type in this area and the geological conditions
are analyzed by the statistics of the physical parameters. Then,
the tectonic, rocks, stratum, ore geophysical models have been
treated by the forward modeling numerical simulation and the
results are analyzed comprehensively. Based on the forward modeling
results, combined with the relevant physical differences, the
principle and exploration method test and research for the comprehensive
geophysical exploration technology has been carried out, covering
the induced polarization and magnetic prospecting for the ore
body as well as the indirect geophysical exploration method
by means of plane gravity data, audio-magnetotelluric sounding
for rock mass and tectonics, the mineralization mode-physical
forward modeling - geophysical exploration mode has been established
and good results have been achieved. Therefore, a location forecast
method has been put forward for the concealed skarn type Fe-Au
deposit which is adaptive to the mineralized geological background
of Beiya and other similar areas.
Keywords: Beiya gold ore; forward modeling; prospecting model
ABSTRAK
Menurut peraturan asas dan ciri timbunan polilogam emas di kawasan lombong
emas Beiya daripada segi mineralisasi dan pengawalan bijih,
dapat disimpulkan bahawa timbunan skarn adalah timbunan bijih
utama di kawasan ini dan keadaan geologinya dianalisis oleh
parameter fizikal statistik. Seterusnya, model tektonik, batuan,
strata dan geofizik bijih telah dirawat menggunakan model ke
hadapan simulasi berangka dan hasilnya dianalisis secara menyeluruh.
Berdasarkan hasil pemodelan ke hadapan, digabungkan dengan perbezaan
fizikal yang relevan, kaedah pengujian dan penyelidikan prinsip
dan eksplorasi untuk teknologi eksplorasi geofizik yang komprehensif
telah dijalankan, meliputi kaedah polarisasi teraruh dan pencarigalian
magnet untuk jisim bijih serta kaedah penerokaan geofizik tidak
langsung dengan menggunakan data graviti pesawat, bunyi magnetotellurik
untuk jisim batuan dan tektonik, mod mineralisasi - pemodelan
fizikal ke hadapan - mod penerokaan geofizik telah dibentuk
dan keputusan yang baik telah dicapai. Oleh itu, kaedah ramalan
lokasi dikemukakan bagi mengesean timbunan skarn jenis Fe-Au
tersembunyi yang mudah sesuai dengan latar belakang geologi
mineral di kawasan Beiya dan kawasan yang sama.
Kata kunci : bijih emas Beiya; model
pencarigalian; pemodelan ke hadapan
REFERENCES
Brian, S.A., Mark, E.W. & Jogn,
E.B. 1998. A Report on the Renaissance of Gravity in the
Deep Water Gulf of Mexico: A Practical View of Integration Methods.
In annual meeting abstracts. Society of Exploration Geophysicists.
pp. 515-517.
Camacho, A.G., Montesinos, F.G.
& Vieira, R. 2002. A 3-D gravity inversion tool based on
exploration of model possibilities. Computers & Geosciences
28(2): 191-204.
Grechka, V., Theophanis, S. &
Tsvankin, I. 1999. Joint inversion of P-and Ps-waves in orthorhombic
media: Theory and a physical-modeling study. Geophysics 66(1):
146-161.
He, Z.H., Zhou, Y.M. & He, W.Y.
2013. Genetic types and metallogenic regularity of Beiya superlarge
gold-polymetallic deposit, northwestern Yunnan. Mineral Deposits
32(2): 244-258.
Huang, N.E. 2006. An adaptive data
analysis method for nonlinear and nonstationary time series:
The empirical mode decomposition and Hilbert spectral analysis.
Applied and Numerical Harmonic Analysis. Switzer-land:
Brikhauser Verlag Basel. pp. 63-37.
Li, J., Ding, J. & Niu, H.B.
2016. Geochemical characteristics of magnetite from Beiya gold
polymetallic deposit in western Yunnan and its constraint on
mineralization. Mineral Deposits 35(2): 395-413.
Liu, G.D. & Hao, T.Y. 1995.
Searching of hidden mineral deposits by geophysical methods.
Chinese Journal of Geophysics 6: 618-626.
Liu, J.X., Sun, H.L. & Chen,
B. 2016. Review of the gravity and magnetic methods in the exploration
of metal deposits. Progress in Geophysics 31(2): 713-722.
Rossi, G. & Vesnaver, A. 1997.
3-D imaging by adaptive joint inversion of reflected and refracted
arrivals. In Annual Meeting Abstracts. Society of Exploration
Geophysicists. pp. 1873-1876.
Sirajuddin, N.A. & Md. Jamil
M.S. 2015. Self-healing of poly (2-hydroxyethyl methacrylate)
hydrogel through molecular diffusion. Sains Malaysiana 44(6):
811-818.
Sultana, M.N., Akib, S. & Ashraf,
M.A. 2017. Thermal comfort and runoff water quality performance
on green roofs in tropical conditions. Geology, Ecology,
and Landscapes 1(1): 47-55.
Wu, H., Zhao, B. & Gao, W. 2017.
Analysis of gradient descent ontology iterative algorithm for
geological setting. Geology, Ecology, and Landscapes 1(1):
41-46.
Xiao, K.Y., Zhu, Y.S. & Zhang,
X.H. 1999. The extraction and integration technology of minerogenic
information in mineral resource assessment. Mineral Doposits
18(4): 379-384.
Yang, C.H., Tong, L.T. & Huang,
C.F. 1999. Combined application of DC and TEM to sea-water intrusion
mapping. Geophysics 64(2): 417-425.
Yin, F.G.,
Sun, Z.M., & Ren, G. 2012. Geological record of paleo-and
mesoproterozoic orogenesis in the western margin of upper Yangtze
block. Acta Geologica Sinica 86: 1918-1932.
Zeng, Q.Q. & Liu, T.Y. 2010.
A potential field separation method based on empirical mode
decomposition. Oil Geophysical Prospecting 45: 914-918.
*Corresponding author; email: 115138871@qq.com