Aquifer permeability change caused by a near-field earthquake, Canterbury, New Zealand-Reference-Cited by-同舟云学术

Aquifer permeability change caused by a near-field earthquake, Canterbury, New Zealand

Published:2016-11 Issue:11 Volume:52 Page:8861-8878
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Rutter H. K.¹^ORCID,Cox S. C.²^ORCID,Dudley Ward N. F.³,Weir J. J.¹

Affiliation:

1. Aqualinc Research Ltd; Christchurch New Zealand

2. GNS Science; Dunedin New Zealand

3. Department of Civil and Natural Resource Engineering; University of Canterbury; Christchurch New Zealand

Funder

Royal Society of New Zealand Marsden

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015WR018524/fullpdf

Reference61 articles.

1. Valley fills and coastal cliffs buried beneath an alluvial plain: Evidence from variation of permeabilities ingravel aquifers, Canterbury Plains, New Zealand;Bal;J. Hydrol. N. Z.,1996

2. The Darfield (Canterbury) earthquake: Geodetic observations and preliminary source model;Beavan;Bull. N. Z. Soc. Earthquake Eng.,2010

3. Bidwell , V. J. 2003 MAF Tech. Pap. 2003/6 http://www.maf.govt.nz/mafnet/rural-nz/sustainable-resource-use/water-efficiency/groundwater-management-tools/tech-paper-0306-groundwater-management-tools.pdf

4. Bidwell , V. J. M. J. Morgan 2002

5. A mechanism for sustained groundwater pressure changes induced by distant earthquakes;Brodsky;J. Geophys. Res.,2003

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