Analytical predictions for a natural spacing within dyke swarms

被引:24
作者
Bunger, Andrew P. [1 ,2 ]
Menand, Thierry [3 ,4 ,5 ]
Cruden, Alexander [6 ]
Zhang, Xi [2 ]
Halls, Henry [7 ]
机构
[1] Univ Pittsburgh, Dept Civil & Environm Engn, Pittsburgh, PA 15261 USA
[2] CSIRO Earth Sci & Resource Engn, Melbourne, Vic, Australia
[3] Univ Blaise Pascal, Lab Magmas & Volcans, Clermont Univ, Clermont Ferrand, France
[4] LMV, CNRS, UMR 6524, Clermont Ferrand, France
[5] LMV, IRD, R 163, Clermont Ferrand, France
[6] Monash Univ, Sch Geosci, Melbourne, Vic 3004, Australia
[7] Univ Toronto, Dept Chem & Phys Sci, Mississauga, ON, Canada
关键词
dyke swarms; dyke spacing; fluid-driven cracks; hydraulic fractures; KAPUSKASING STRUCTURAL ZONE; HYDRAULIC-FRACTURE; CRACK-PROPAGATION; MAGMA TRANSPORT; KILAUEA VOLCANO; DIKE SWARMS; KRAFLA; DISTRIBUTIONS; DEFORMATION; EMPLACEMENT;
D O I
10.1016/j.epsl.2013.05.044
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Dykes often grow next to other dykes, evidenced by the widespread occurrence of dyke swarms that comprise many closely spaced dykes. In giant dyke swarms, dykes are observed to maintain a finite spacing from their neighbors that is tens to hundreds of times smaller than their length. To date, mechanical models have not been able to clarify whether there exists an optimum or natural spacing between the dykes. And yet, the existence of a natural spacing is at the heart of why dykes grow in swarms in the first place. Here we present and examine a mechanical model for the horizontal propagation of multiple, closely spaced blade-like dykes in order to find energetically optimal dyke spacings associated with both constant pressure and constant influx magma sources. We show that the constant pressure source leads to an optimal spacing that is equal to the height of the blade-like dykes. We also show that the constant influx source leads to two candidates for an optimal spacing, one which is expected to be around 0.3 times the dyke height and the other which is expected to be around 2.5 times the dyke height. Comparison with measurements from dyke swarms in Iceland and Canada lends initial support to our predictions, and we conclude that dyke swarms are indeed expected to have a natural spacing between first generation dykes and that this spacing scales with, and is on the order of, the height of the blade-like dykes that comprise the swarm. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:270 / 279
页数:10
相关论文
共 70 条
[1]   Asymptotic analysis of an elasticity equation for a finger-like hydraulic fracture [J].
Adachi, Jose I. ;
Peirce, Anthony P. .
JOURNAL OF ELASTICITY, 2008, 90 (01) :43-69
[2]  
AMand Rubin., 1987, Volcanism in Hawaii, V1350, P1449
[3]   September 2005 mega-dike emplacement in the Manda-Harraro nascent oceanic rift (Afar depression) [J].
Ayele, Atalay ;
Keir, Derek ;
Ebinger, Cynthia ;
Wright, Tim J. ;
Stuart, Graham W. ;
Buck, W. Roger ;
Jacques, Eric ;
Ogubazghi, Ghebrebrhan ;
Sholan, Jamal .
GEOPHYSICAL RESEARCH LETTERS, 2009, 36
[4]   Fracture spacing in layered rocks: a new explanation based on the stress transition [J].
Bai, TX ;
Pollard, DD .
JOURNAL OF STRUCTURAL GEOLOGY, 2000, 22 (01) :43-57
[5]   Longitudinal petrochemical variation in the Mackenzie dyke swarm, Northwestern Canadian shield [J].
Baragar, WRA ;
Ernst, RE ;
Hulbert, L ;
Peterson, T .
JOURNAL OF PETROLOGY, 1996, 37 (02) :317-359
[6]   BROAD-SCALE PROTEROZOIC DEFORMATION OF THE CENTRAL SUPERIOR-PROVINCE REVEALED BY PALEOMAGNETISM OF THE 2.45 GA MATACHEWAN DYKE SWARM [J].
BATES, MP ;
HALLS, HC .
CANADIAN JOURNAL OF EARTH SCIENCES, 1991, 28 (11) :1780-1796
[7]  
Benthem J. P., 1973, Mechanics of fracture. Vol.1: Methods of analysis and solutions of crack problems, P131
[8]   SEISMIC ACTIVITY ASSOCIATED WITH THE SEPTEMBER 1977 DEFLATION OF THE KRAFLA CENTRAL VOLCANO IN NORTHEASTERN ICELAND [J].
BRANDSDOTTIR, B ;
EINARSSON, P .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1979, 6 (3-4) :197-212
[9]   THERMAL CONTROL OF BASALTIC FISSURE ERUPTIONS [J].
BRUCE, PM ;
HUPPERT, HE .
NATURE, 1989, 342 (6250) :665-667
[10]   Analysis of the power input needed to propagate multiple hydraulic fractures [J].
Bunger, A. P. .
INTERNATIONAL JOURNAL OF SOLIDS AND STRUCTURES, 2013, 50 (10) :1538-1549