Quantitative geometric description of fracture systems in an andesite lava flow using terrestrial laser scanner data

被引:12
|
作者
Massiot, Cecile [1 ,4 ]
Nicol, Andrew [2 ]
Townend, John [1 ]
McNamara, David D. [3 ,4 ]
Garcia-Selles, David [5 ]
Conway, Chris E. [1 ,6 ]
Archibald, Garth [4 ]
机构
[1] Victoria Univ Wellington, POB 600, Wellington 6012, New Zealand
[2] Univ Canterbury, Christchurch, New Zealand
[3] Natl Univ Ireland, Sch Nat Sci, Earth & Ocean Sci, Univ Rd, Galway, Ireland
[4] Avalon, GNS Sci, POB 30-368, Lower Hutt 5040, New Zealand
[5] Univ Barcelona, Barcelona, Spain
[6] Natl Museum Nat & Sci, Dept Geol & Paleontol, 4-1-1 Amakubo, Tsukuba, Ibaraki 3050005, Japan
关键词
Fracture system; Andesite lava flow; Terrestrial laser scanner; Ruapehu volcano; TAUPO VOLCANIC ZONE; HIGH-RESOLUTION; NEW-ZEALAND; FLUID-FLOW; RUAPEHU VOLCANO; OUTCROP; EVOLUTION; RESERVOIR; MODELS; PERMEABILITY;
D O I
10.1016/j.jvolgeores.2017.05.036
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Permeability hosted in andesitic lava flows is dominantly controlled by fracture systems, with geometries that are often poorly constrained. This paper explores the fracture system geometry of an andesitic lava flow formed during its emplacement and cooling over gentle paleo-topography, on the active Ruapehu volcano, New Zealand. The fracture system comprises column-forming and platy fractures within the blocky interior of the lava flow, bounded by autobreccias partially observed at the base and top of the outcrop. We use a terrestrial laser scanner (TLS) dataset to extract column-forming fractures directly from the point-cloud shape over an outcrop area of similar to 3090 m(2). Fracture processing is validated using manual scanlines and high resolution panoramic photographs. Column-forming fractures are either steeply or gently dipping with no preferred strike orientation. Geometric analysis of fractures derived from the TLS, in combination with virtual scanlines and trace maps, reveals that: (1) steeply dipping column-forming fracture lengths follow a scale-dependent exponential or log-normal distribution rather than a scale-independent power-law; (2) fracture intensities (combining density and size) vary throughout the blocky zone but have similar mean values up and along the lava flow; and (3) the areal fracture intensity is higher in the autobreccia than in the blocky zone. The inter-connected fracture network has a connected porosity of similar to 0.5 % that promote fluid flow vertically and laterally within the blocky zone, and is partially connected to the autobreccias. Auto-breccias may act either as lateral permeability connections or barriers in reservoirs, depending on burial and alteration history. A discrete fracture network model generated from these geometrical parameters yields a highly connected fracture network, consistent with outcrop observations. (C) 2017 Elsevier B.V. All rights reserved.
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页码:315 / 331
页数:17
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