Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Alpine Fault
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
=== Deep Fault Drilling Project === The Deep Fault Drilling Project (DFDP) was an attempt in 2014 to retrieve rock and fluid samples and make geophysical measurements inside the Alpine Fault zone at depth.<ref>{{Cite journal|last=Townend|first=John|date=2009|title=Deep Fault Drilling Project—Alpine Fault, New Zealand|url=https://www.sci-dril.net/8/75/2009/sd-8-75-2009.pdf|journal=Scientific Drilling|volume=8|pages=75–82|doi=10.5194/sd-8-75-2009|bibcode=2009SciDr...8...75T |doi-access=free}}</ref><ref name="phys.org">{{Cite web|url=https://phys.org/news/2014-09-drilling-earthquake-fault-zealand.html|title=Drilling into an active earthquake fault in New Zealand|website=phys.org|access-date=2019-02-16}}</ref> It was a $2.5 million international research project designed to drill 1.3 km to the fault plan in two months.<ref name="phys.org" /> The DFDP was the second project to try to drill an active fault zone and return samples after the [[San Andreas Fault Observatory at Depth]].<ref name="phys.org" /><ref>{{Cite news|url=https://www.theguardian.com/science/2005/dec/10/thisweekssciencequestions.geology|title=Why are scientists drilling into the San Andreas fault?|last=Ravilious|first=Kate|date=2005-12-10|work=[[The Guardian]] |access-date=2018-12-31|issn=0261-3077}}</ref> One of the goals of the project was to use the deformed rocks from the fault zone to determine its resistance to stress.<ref name="phys.org" /> Researchers also planned to install long term equipment for measuring pressure, temperature and seismic activity near the fault zone.<ref name="phys.org" /> It was led by New Zealand geologists [[Rupert Sutherland]], John Townsend and [[Virginia Toy]] and involves an international team from New Zealand, Canada, France, Germany, Japan, the United Kingdom, and the United States.<ref>{{Cite web|url=https://www.gns.cri.nz/Home/News-and-Events/Media-Releases/drill-probe-in-Alpine-Fault/DEEP-FAULT-DRILLING-PROJECT-2-FAQs|title=DEEP FAULT DRILLING PROJECT-2 FAQs / drill probe in Alpine Fault / Media Releases / News and Events / Home – GNS Science|website=gns.cri.nz|access-date=2018-12-31}}</ref> In 2017, they reported they had discovered beneath [[Whataroa]], a small township on the Alpine Fault, "extreme" hydrothermal activity which "could be commercially very significant".<ref name="Sutherland2017"/><ref>{{cite web|url=https://www.odt.co.nz/regions/west-coast/geothermal-discovery-west-coast|title=Geothermal discovery on West Coast|date=18 May 2017|website=[[Otago Daily Times]] }}</ref> One of the lead researchers said that it is likely to be globally unique.<ref>{{Cite news|url=https://www.nzherald.co.nz/the-country/news/article.cfm?c_id=16&objectid=11858291|title=Geothermal discovery on West Coast|last=Elder|first=Vaughan|work=[[The New Zealand Herald]] |access-date=2018-12-30|issn=1170-0777}}</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)