The Rock Mechanics of Kimberlite Volcanic Pipe Evacuation

Author(s): 
Wayne Barnett
Date: 
Tuesday, December 11, 2007
First presented: 
Journal of Volcanology and Geothermal Research
Type: 
Published paper
Category: 
Geology

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Abstract

The rock mechanics theory for deformation of open pit and underground mining excavations can be used to better understand aspects of the growth and geometry of kimberlite volcanic pipes. Large scale rock mass behaviour around an excavation, such as a volcanic pipe, is dependent on the rock mass strength, the in-situ rock stress conditions and the excavation geometry. Rock mass strength is empirically derived from the intact rock strength and quantification of the shear strength, frequency and orientation of rock discontinuities. Tensile slope or sidewall failure typically occurs in shallow level (~0 – 1000 m) conditions in which pre-existing structures shear due to gravity-driven forces. The orientation of the pre-existing structures provides an important control on the size, shape and position of the rock mass failure. Slope failures are shown to influence the development of many kimberlite volcanic craters and the distribution of layered volcaniclastic facies in the crater. Explosions or removal of key- blocks in a pipe sidewall can cause undercutting and collapse of the sidewall, with the rock unravelling along pre-existing structures towards surface. Many lithic-rich breccias commonly found on the margins of kimberlite pipes are interpreted to form in this way. At intermediate (>1000 m) to deep (>2500 m) depths, the increasing compressive stress can cause fractures to develop around an excavation. Stress-induced fractures should cause scaling of a volcanic pipe's sidewalls and expansion perpendicular to the maximum component of compressive stress. A larger horizontal tectonic stress ratio and a lower internal pipe pressure will promote pipe sidewall fracturing. Volcanic pipe expansion will also be increased in rate by (i) mechanical sidewall erosion by flowing magma and/or pyroclasts, (ii) by failure on large intersecting fault or dyke structures, and (iii) by reduction in the country rock mass strength by volcanic explosions. The final pipe shape and distribution of some internal facies is therefore a consequence of the dominant rock mechanical failure processes in the pipe sidewalls. The type of failure is dependant on the rock mass strength, geological structures, stress and depth below surface.

© 2008 Elsevier B.V. All rights reserved.

Feature Author

Dr. Wayne Barnett

Wayne Barnett has 18 years of experience in the mining and exploration industry. He specializes in providing operational support by defining the structural geology of mining projects and properly characterizing their rock masses in order to manage risks and solve problems in active mining operations. He also characterizes the structural geology for scoping- to feasibility-level studies.

Wayne has a PhD in structural geology and industry certification in rock mechanics, and worked as a geotechnical engineer for two mining operations over a period of 8 years.

Principal Structural Geologist
PhD, PrSciNat
SRK Vancouver
SRK Turkey