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UNIT 14
EXPLORATION METHODS
Structure______________________________________________
14.1 Introduction Self-Potential Method
Expected Learning Outcomes Telluric Current Method
14.2 Exploration Methods Magnetotelluric Method
14.3 Surface Exploration Resistivity Method
Geological Exploration Induced Potential Method
Photogeology, Remote Sensing Electromagnetic Method
and Geographic Information Seismic Method
System
Geochemical Exploration Pitting, Trenching, Drilling and
Borehole Logging
Geobotanical Exploration 14.5 Activity
Biogeochemical Survey 14.6 Summary
14.4 Subsurface Exploration 14.7 Terminal Questions
Methods
Gravity Method 14.8 References
Magnetic Method 14.9 Further/Suggested Readings
Electrical Method 14.10 Answers
14.1 INTRODUCTION
In the previous unit, you have studied about basic principles and stages of mineral exploration.
Mineral exploration has its own characteristic and is dominated by “High Risk-High Reward”
proposition as the occurrence of mineral deposit is not uniform worldwide. In this unit, you will learn
about different mineral exploration methods that involve various activities to identify/ quantify and
extract economically hidden deposits to the surface. The physicochemical properties of the minerals
like specific gravity, electrical conductivity, magnetic susceptibility, radioactivity, propagation of
seismic waves and mode of occurrence of minerals enables in locating ore deposits of economic
interest.
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Expected Learning Outcomes_______________________
After reading this unit you should be able to:
❖ outline different exploration methods for mineral exploration;
❖ learn principles and practices of exploration methods;
❖ discuss their importance in various stages of mineral exploration; and
❖ explain limitations of each exploration method.
14.2 EXPLORATION METHODS
In the previous Unit 13, you have been introduced to prospecting and
exploration. Now, let us discuss about exploration methods. Different types of
exploration methods are essential to find out and estimate volume of a
commercially viable mineral concentration as it involves high capital-intensive
operations. The exploration methods are divided into two main groups, namely:
A) Surface exploration; and
B) Subsurface exploration.
Involvement of different surface and subsurface exploration methods during
various stages of mineral exploration projects is shown in Figure 14.1. Surface
exploration methods includes: geological, geochemical, geobotanical,
photogeology & remote sensing. Subsurface exploration methods include:
gravity, magnetic, electrical, self-potential, telluric current, magnetotelluric,
resistivity, induced potential, electromagnetic, seismic. We will discuss the
surface and subsurface exploration methods in details in the following sections.
Fig. 14.1: Types of mineral exploration methods.
14.3 Surface Exploration
The surface exploration method includes preparation of geological maps based
on data collected through field survey (including elevation data). Incorporation
of aerial photos, satellite imagery, geochemical and vegetation data into these
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Unit 14 Exploration Methods
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maps provide useful details regarding rock outcrops and their boundaries,
vegetation, geomorphology, lithology and lithological variations of the area
under investigation. Various surface exploration methods viz. geological,
geochemical, geobotanical, photogeology and remote sensing are carried out
during preliminary & detailed survey.
Let us discuss them in the following sections.
14.3.1 Geological Exploration
The occurrence of ore bodies are mainly controlled by geologic setting with
specific structural and tectonic setting and their spatial distribution over a wide
area.
Selection of most prospective area for exploration requires a sound geological
knowledge which includes structure of the area, age of the rocks, rock types
and basin modelling etc. Good acquaintance is required to make perfect
predictions and draw parallels between an established ore deposit and the
unknown potential mineralisation sought after exploration. The broad activities
involved in geological exploration are:
• to prepare a field database from different sources; and
• plot in geological base map.
The detailed activities include:
i) Review of existing data and field work: The exploration begins with the
regional appraisal of large area through available geological information,
review of literature, earlier published maps, survey and reports from different
sources. After preliminary findings from the review, the exploration team
visits the field to gather information related to geological, mineralisation, host
rock and hunting for the surface guides to incorporate and prepare the
geological base map for next phase of exploration.
ii) Geological / Surface Guides: During geological traverse, the exploration
team explores the existence of various types of surface signatures of mineral
deposits called geological or surface guides. You have read about
geological / surface guides in the previous Unit 13.
iii) Study of Topographic Maps: A topographical map (toposheets or
topomaps) commonly shows quantitative and precise representation of
physical and cultural features of the Earth’s surface. They represent a
symbolic picture of the natural and man-made features of small areas which
are drawn at relatively large scale (Fig.14.2). As a result, these maps serve
as indispensable tool for city and regional planners, natural resources
managers, and for engineering, environmental and geological studies. Earlier
a topographic survey is conducted with tape and compass. Now a days, it is
being done using electronic total stations to capture 3D observation data on
the field to prepare digital terrain model that is transformed into a high quality
geological map.
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Fig. 14.2: Topographic maps (a) 1:250000; (b) 1: 50000 and (c) 1: 25000 scales.
(Source: www.surveyofindia.gov.in)
The activities carried out during geological exploration can be subdivided into
three main categories namely regional scale, belt scale and deposit scale.
• Regional Scale: Surface features, like broad geological contacts,
existence of shear zones and weathering features are regionally plotted in
the base map. Study of aerial photographs, satellite images, airborne
geophysical data acquisition, wide spaced soil sample, grab and chip
sampling of surface exposures for broad geochemical surveys and
weathering profiles are collected and recorded.
• Mineral Belt Scale: Geological base map survey is scaled up to 1:25000
or 1:10000 scales using theodolite and GPS survey instruments. Detailed
study of geological structural setting such as stratigraphy and
identification of host rock, surface shows of mineralisation, existence of
ancient mining and smelting signatures are recorded and plotted in the
base map. Additionally, ground geophysics, geochemistry, pitting,
trenching data are acquired for data integration.
• Mineral Deposit Scale: After integrated study of the area, maximum
information of the mineral deposit is acquired by triangulation station
survey. Thereafter, base map in larger scale of 1:5000 or 1:1000 is
prepared. Additionally, closely spaced surface drilling, trenches, pits and
boreholes is carried out along and across the mineral body to delineate
and extension of the mineral deposit (Fig. 14.3).
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