Featured Research

from universities, journals, and other organizations

Earthquakes Reveal Diamonds' Origins

Date:
July 18, 2001
Source:
Arizona State University College Of Liberal Arts & Sciences
Summary:
The seismic rumblings could provide key clues about where miners should look for diamonds, according to recent research. Matt Fouch, assistant professor of geological sciences at ASU, studies vibrations caused by earthquakes to visualize the earth at depths of hundreds of kilometers, where diamonds are formed. His maps of the earth below South Africa provide new information about Earth’s structure in regions where many diamonds are found.

The seismic rumblings could provide key clues about where miners should look for diamonds, according to recent research. Matt Fouch, assistant professor of geological sciences at ASU, studies vibrations caused by earthquakes to visualize the earth at depths of hundreds of kilometers, where diamonds are formed. His maps of the earth below South Africa provide new information about Earth’s structure in regions where many diamonds are found.

Related Articles


In the July 1, 2001 issue of Geophysical Research Letters, Fouch and his coauthors, David James, John VanDecar (both of the Department of Terrestrial Magnetism, Carnegie Institution of Washington), and Suzan van der Lee (of the Institute of Geophysics, Zόrich, Switzerland), show that some of southern Africa’s most profitable diamond mines are located near areas where the earth is exceptionally stable and cool up to 250 kilometers below the surface. The paper will be published in a special section of the journal, with seven other studies on geochemistry, composition, and rock dating of southern Africa.

Many diamonds come from regions, called cratons, that are some of the most geologically stable places in the world. Two cratons, the Kaapvaal and Zimbabwe cratons, covering an area roughly the size of the nation of South Africa, are the source of most of southern Africa's diamonds.

"The region we're studying in southern Africa is over 3 billion years old, and in some places it's even 3.6 billion years old," says Fouch. Geologists think diamonds develop up to several hundred kilometers deep within these ancient cratons and are then driven straight up to the surface.

Miners scout the best places to dig for gems by looking for diamonds that have made their way to the surface. Other techniques, such as drilling for samples deeper in the rock or studying anomalies in the gravitational or magnetic properties of the earth in the area, increase the chances of finding diamonds. But none of these approaches guarantee success. "If people knew exactly how it worked all the time, then we'd have a lot more diamond mines," Fouch jokes. "Nearly all diamonds come from cratons, but not all cratons contain diamonds. So the question is, why do some cratons produce diamonds and others don't? Another question is, why do some of those areas have diamonds that are commercially profitable, and others don't? Some regions have diamonds, but they're just too chewed up to be gem quality."

Fouch and his colleagues think they may have found part of the answer deep in the earth's mantle -- the layer of rock that extends several hundred kilometers beneath the crust. By imaging the earth at these depths, they looked at the very source of diamonds, rather than waiting for them to travel to the surface.

Fouch created three-dimensional images of deep layers of the earth by using an array of 82 seismometers, sensors that detect vibrations caused by earthquakes from all around the world. The seismometers, placed at roughly 100-kilometer intervals across South Africa, Zimbabwe and Botswana, recorded data from more than 200 earthquakes occurring over a two-year period, mainly from the Himalayan and Andean mountain ranges. They used seismic tomography, a technique very similar to CAT scans in medical imaging, to produce the images.

"As people, we never want earthquakes to happen, but as seismologists we know they are an inevitability. So our job is to use them in the most productive way possible," says Fouch. "Every time an earthquake happens, it's like shining a flashlight on a particular part of the earth. The seismic waves from each earthquake bounce off of different layers of the earth and illuminate different internal features."

The speed and angle of earthquake waves' motion depends on what kind of material they travel through. For example, the rippling caused by dropping a pebble in a bowl of water will move differently than in water containing ice cubes or in a bowl of jelly. By analyzing the timing and angle of the vibrations' spread past the seismometers, Fouch and coworkers mapped the physical properties of the earth below.

They found that the mantle directly below the most productive diamond mines looks distinctly different than in the surrounding areas. In diamond-producing areas, the mantle is "seismically fast," meaning that it propagates earthquake vibrations quickly because the mantle rock may be cooler or chemically different from the surrounding areas.

"There are a few distinct pockets of the faster seismic velocities," Fouch explains. "One of these regions is beneath the Kaapvaal craton in South Africa, and one -- a little more diffuse -- is beneath the Zimbabwe craton. ... Most of the gem-quality diamond mines in southern Africa lie very close to these regions." By looking for similarly cold, seismically fast parts of the mantle, diamond miners may be able to identify new promising areas for mining.

Industry collaborators in southern Africa are very interested in Fouch's research, and some even allowed the seismologists to install seismometers on their property.

"This is certainly a technique that could be used in conjunction with other methods to possibly determine whether a region might be more prone to having diamonds," Fouch says.


Story Source:

The above story is based on materials provided by Arizona State University College Of Liberal Arts & Sciences. Note: Materials may be edited for content and length.


Cite This Page:

Arizona State University College Of Liberal Arts & Sciences. "Earthquakes Reveal Diamonds' Origins." ScienceDaily. ScienceDaily, 18 July 2001. <www.sciencedaily.com/releases/2001/07/010717081100.htm>.
Arizona State University College Of Liberal Arts & Sciences. (2001, July 18). Earthquakes Reveal Diamonds' Origins. ScienceDaily. Retrieved October 24, 2014 from www.sciencedaily.com/releases/2001/07/010717081100.htm
Arizona State University College Of Liberal Arts & Sciences. "Earthquakes Reveal Diamonds' Origins." ScienceDaily. www.sciencedaily.com/releases/2001/07/010717081100.htm (accessed October 24, 2014).

Share This



More Earth & Climate News

Friday, October 24, 2014

Featured Research

from universities, journals, and other organizations


Featured Videos

from AP, Reuters, AFP, and other news services

EU Gets Climate Deal, UK PM Gets Knock

EU Gets Climate Deal, UK PM Gets Knock

Reuters - Business Video Online (Oct. 24, 2014) — EU leaders achieve a show of unity by striking a compromise deal on carbon emissions. But David Cameron's bid to push back EU budget contributions gets a slap in the face as the European Commission demands an extra 2bn euros. David Pollard reports. Video provided by Reuters
Powered by NewsLook.com
Deep Sea 'mushroom' Could Be Early Branch on Tree of Life

Deep Sea 'mushroom' Could Be Early Branch on Tree of Life

Reuters - Innovations Video Online (Oct. 24, 2014) — Miniature deep sea animals discovered off the Australian coast almost three decades ago are puzzling scientists, who say the organisms have proved impossible to categorise. Academics at the Natural History of Denmark have appealed to the world scientific community for help, saying that further information on Dendrogramma enigmatica and Dendrogramma discoides could answer key evolutionary questions. Jim Drury has more. Video provided by Reuters
Powered by NewsLook.com
Raw: Tornado Rips Roofs in Washington State

Raw: Tornado Rips Roofs in Washington State

AP (Oct. 24, 2014) — A rare tornado ripped roofs off buildings, uprooted trees and shattered windows Thursday afternoon in the southwest Washington city of Longview, but there were no reports of injuries. (Oct. 24) Video provided by AP
Powered by NewsLook.com
Fast-Moving Lava Headed For Town On Hawaii's Big Island

Fast-Moving Lava Headed For Town On Hawaii's Big Island

Newsy (Oct. 24, 2014) — Lava from the Kilauea volcano on Hawaii's Big Island has accelerated as it travels toward a town called Pahoa. Video provided by Newsy
Powered by NewsLook.com

Search ScienceDaily

Number of stories in archives: 140,361

Find with keyword(s):
 
Enter a keyword or phrase to search ScienceDaily for related topics and research stories.

Save/Print:
Share:  

Breaking News:

Strange & Offbeat Stories

 

Plants & Animals

Earth & Climate

Fossils & Ruins

In Other News

... from NewsDaily.com

Science News

Health News

Environment News

Technology News



Save/Print:
Share:  

Free Subscriptions


Get the latest science news with ScienceDaily's free email newsletters, updated daily and weekly. Or view hourly updated newsfeeds in your RSS reader:

Get Social & Mobile


Keep up to date with the latest news from ScienceDaily via social networks and mobile apps:

Have Feedback?


Tell us what you think of ScienceDaily -- we welcome both positive and negative comments. Have any problems using the site? Questions?
Mobile iPhone Android Web
Follow Facebook Twitter Google+
Subscribe RSS Feeds Email Newsletters
Latest Headlines Health & Medicine Mind & Brain Space & Time Matter & Energy Computers & Math Plants & Animals Earth & Climate Fossils & Ruins