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Ocean-drilling Expedition Cites New Evidence Related To Origin And Evolution Of Seismogenic Faults
ScienceDaily (Aug. 21, 2009) — New research about what triggers earthquakes, authored by Michael Strasser of Bremen University, Germany, with colleagues from the USA, Japan, China, France, and Germany, will appear in the Aug. 16 2009 issue of Nature Geoscience (online version). The research article, titled "Origin and evolution of a splay-fault in the Nankai accretionary wedge" is drawn from the scientists' participation in the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE), a long-term scientific ocean-drilling project conducted by the Integrated Ocean Drilling Program (IODP).
See also:
Earth & Climate
* Earthquakes
* Natural Disasters
* Geology
* Oceanography
* Geography
* Tsunamis
Reference
* North Anatolian Fault
* Geologic fault
* Oceanic trench
* Alpine Fault
Since September 2007, rotating teams of scientists have spent months aboard Japan's drilling vessel, CHIKYU, investigating the Nankai Trough, a seismogenic zone located beneath the ocean off the southwest coast of Japan. Drilling operations, managed by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) through its Center for Deep Earth Exploration, have resulted in a collection of cored samples from the sea floor, which have provided scientists with deeper insights into the geologic past of the area.
Discussion in the above-noted article focuses on the Nankai Trough, in which the Philippine Sea plate slips below the Eurasian Plate with a velocity of 4 cm per year. This area is one of the most active earthquake zones on the planet. While being subducted, sediments are scraped off the oceanic plate and added to the overriding continental plate. Due to the movement of the plates these so-called accretionary wedges are exposed to enormous stress that form large faults. The landward wedge in the Nankai Trough is completely intersected by such a prominent fault which extends laterally over more than 120 km. Scientists refer to this structure as "the megasplay." Movements along such megasplay faults during large magnitude earthquakes generated at depth may rupture the ocean floor and generate tsunamis.
"Our knowledge of megasplay faults up till now has been based on seismic or modelling experiments accomplished over the last twenty years," says Michael Strasser of Post-Doc Fellow of the Center for Marine Environmental Sciences (MARUM) at University of Bremen. "For the first time, with cored samples brought onto the CHIKYU, it has become possible to reconstruct the geological history of a fault in great detail." With his associates, Dr. Strasser found that the fault in the Nankai Trough originated about two million years ago. From the information recorded in the cores, the research team can draw conclusions on the mechanics of the accretionary wedge. They also can infer in which geological time periods the fault was most active.
"Our most significant conclusion is that splay fault activity varies through time," Dr. Strasser states. According to Strasser, after an initial period of high activity, the movement along the fault slowed down. Since about 1.55 million years ago, this fault has been reactivated, favoring ongoing megasplay slip along it.
"It is absolutely fascinating to be part of NanTroSEIZE," says Strasser, noting that the expedition series aims to sample and monitor activity at the point where earthquakes originate. "NanTroSEIZE is something completely new and innovative in scientific drilling," Strasser explains. "Ultimately, we hope to detect signals occurring just before an earthquake to get a better understanding of the processes leading to earthquakes and tsunamis."
The Nankai Trough is particularly suited for this experiment because historical records of earthquakes and tsunamis in this area date back into the seventh century. Additionally, the area where earthquakes are generated, the so-called seismogenic zone, is located at a relatively shallow depth of about six kilometers below the seafloor.
In 2007 and 2008, during the first stage of NanTroSEIZE, the deep sea drilling vessel CHIKYU carried out three expeditions. This drilling project consists of four stages in all, and ultimately focuses on "ultra-deep" drilling that can reach the seismogenic zone, where great earthquakes have occurred repeatedly.
During upcoming expeditions, the Nankai Trough boreholes will be equipped with instruments to establish an ocean observatory network. Currently, scientists are making preparations to install monitoring devices for continous measurements of the Nankai Trough. Prof. Gaku Kimura of University of Tokyo, who led an earlier NanTroSEIZE expedition 316 as Co-Chief Scientist says, "Not only do we have new insights about historic fault activities in Nankai Trough, but the data strongly suggests that the megasplay fault may be a key factor in the occurrence of large earthquakes in the future." He adds, "Greater understanding about the processes of earthquake and tsunami generation in the active subduction zone will be a great contribution to society."
Journal reference:
1. Strasser et al. Origin and evolution of a splay fault in the Nankai accretionary wedge. Nature Geoscience, 2009; DOI: 10.1038/ngeo609
Adapted from materials provided by Integrated Ocean Drilling Program Management International, via EurekAlert!, a service of AAAS.
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Integrated Ocean Drilling Program Management International (2009, August 21). Ocean-drilling Expedition Cites New Evidence Related To Origin And Evolution Of Seismogenic Faults. ScienceDaily. Retrieved August 23, 2009, from http://www.sciencedaily.com /releases/2009/08/090817142743.htm
enlarge
The Deep Sea Drilling Vessel Chikyu is the state-of-the-art scientific drill ship operated by the Japan Agency for Marine-Earth Science and Technology through the Center for Deep Earth Exploration for the Integrated Ocean Drilling Program. The NanTroSEIZE Stage 1 expeditions were implemented from September 2007 to February 2008. (Credit: Copyright: JAMSTEC/IODP)
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Related Stories
Locations Of Strain, Slip Identified In Major Earthquake Fault (Feb. 27, 2009) — Deep-sea drilling into one of the most active earthquake zones on the planet is providing the first direct look at the geophysical fault properties underlying some of the world's largest earthquakes ... > read more
Core Samples From Subsea Fault System Off Japan Will Help Explain How Earthquakes Are Generated (Feb. 11, 2008) — Scientists aboard IODP scientific drilling vessel Chikyu collected 5,000 samples from the seismogenic zone known as the Nankai Trough. The samples will provide scientists with new sources of data and ... > read more
Deep-sea Drilling Yields Clues To Mega-earthquakes (Dec. 18, 2007) — Researchers fresh from an eight-week scientific drilling expedition off the Pacific coast of Japan have reported their discovery of strong variation in the tectonic stresses in a region notorious for ... > read more
Small Earthquakes are Useful Predictor of Large Ones (Dec. 5, 2007) — Conventional wisdom in seismology says slip on faults that rupture during the largest continental strike-slip earthquakes is generally limited to the seismogenic layer, the upper 15 km or so of the ... > read more
Deep-sea Scientific Drilling Program To Study Volatile Earthquake Zone Launched (Sep. 25, 2007) — Scientists begin exploring the origins of earthquakes at their source with the launch of the Nankai Trough Seismogenic Zone Experiment. On Sept. 21, the Japanese drilling vessel Chikyu departs from ... > read more
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Ocean-drilling Expedition Cites New Evidence Related To Origin And Evolution Of Seismogenic Faults
ScienceDaily (Aug. 21, 2009) — New research about what triggers earthquakes, authored by Michael Strasser of Bremen University, Germany, with colleagues from the USA, Japan, China, France, and Germany, will appear in the Aug. 16 2009 issue of Nature Geoscience (online version). The research article, titled "Origin and evolution of a splay-fault in the Nankai accretionary wedge" is drawn from the scientists' participation in the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE), a long-term scientific ocean-drilling project conducted by the Integrated Ocean Drilling Program (IODP).
See also:
Earth & Climate
* Earthquakes
* Natural Disasters
* Geology
* Oceanography
* Geography
* Tsunamis
Reference
* North Anatolian Fault
* Geologic fault
* Oceanic trench
* Alpine Fault
Since September 2007, rotating teams of scientists have spent months aboard Japan's drilling vessel, CHIKYU, investigating the Nankai Trough, a seismogenic zone located beneath the ocean off the southwest coast of Japan. Drilling operations, managed by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) through its Center for Deep Earth Exploration, have resulted in a collection of cored samples from the sea floor, which have provided scientists with deeper insights into the geologic past of the area.
Discussion in the above-noted article focuses on the Nankai Trough, in which the Philippine Sea plate slips below the Eurasian Plate with a velocity of 4 cm per year. This area is one of the most active earthquake zones on the planet. While being subducted, sediments are scraped off the oceanic plate and added to the overriding continental plate. Due to the movement of the plates these so-called accretionary wedges are exposed to enormous stress that form large faults. The landward wedge in the Nankai Trough is completely intersected by such a prominent fault which extends laterally over more than 120 km. Scientists refer to this structure as "the megasplay." Movements along such megasplay faults during large magnitude earthquakes generated at depth may rupture the ocean floor and generate tsunamis.
"Our knowledge of megasplay faults up till now has been based on seismic or modelling experiments accomplished over the last twenty years," says Michael Strasser of Post-Doc Fellow of the Center for Marine Environmental Sciences (MARUM) at University of Bremen. "For the first time, with cored samples brought onto the CHIKYU, it has become possible to reconstruct the geological history of a fault in great detail." With his associates, Dr. Strasser found that the fault in the Nankai Trough originated about two million years ago. From the information recorded in the cores, the research team can draw conclusions on the mechanics of the accretionary wedge. They also can infer in which geological time periods the fault was most active.
"Our most significant conclusion is that splay fault activity varies through time," Dr. Strasser states. According to Strasser, after an initial period of high activity, the movement along the fault slowed down. Since about 1.55 million years ago, this fault has been reactivated, favoring ongoing megasplay slip along it.
"It is absolutely fascinating to be part of NanTroSEIZE," says Strasser, noting that the expedition series aims to sample and monitor activity at the point where earthquakes originate. "NanTroSEIZE is something completely new and innovative in scientific drilling," Strasser explains. "Ultimately, we hope to detect signals occurring just before an earthquake to get a better understanding of the processes leading to earthquakes and tsunamis."
The Nankai Trough is particularly suited for this experiment because historical records of earthquakes and tsunamis in this area date back into the seventh century. Additionally, the area where earthquakes are generated, the so-called seismogenic zone, is located at a relatively shallow depth of about six kilometers below the seafloor.
In 2007 and 2008, during the first stage of NanTroSEIZE, the deep sea drilling vessel CHIKYU carried out three expeditions. This drilling project consists of four stages in all, and ultimately focuses on "ultra-deep" drilling that can reach the seismogenic zone, where great earthquakes have occurred repeatedly.
During upcoming expeditions, the Nankai Trough boreholes will be equipped with instruments to establish an ocean observatory network. Currently, scientists are making preparations to install monitoring devices for continous measurements of the Nankai Trough. Prof. Gaku Kimura of University of Tokyo, who led an earlier NanTroSEIZE expedition 316 as Co-Chief Scientist says, "Not only do we have new insights about historic fault activities in Nankai Trough, but the data strongly suggests that the megasplay fault may be a key factor in the occurrence of large earthquakes in the future." He adds, "Greater understanding about the processes of earthquake and tsunami generation in the active subduction zone will be a great contribution to society."
Journal reference:
1. Strasser et al. Origin and evolution of a splay fault in the Nankai accretionary wedge. Nature Geoscience, 2009; DOI: 10.1038/ngeo609
Adapted from materials provided by Integrated Ocean Drilling Program Management International, via EurekAlert!, a service of AAAS.
Email or share this story:
| More
Need to cite this story in your essay, paper, or report? Use one of the following formats:
APA
MLA
Integrated Ocean Drilling Program Management International (2009, August 21). Ocean-drilling Expedition Cites New Evidence Related To Origin And Evolution Of Seismogenic Faults. ScienceDaily. Retrieved August 23, 2009, from http://www.sciencedaily.com /releases/2009/08/090817142743.htm
enlarge
The Deep Sea Drilling Vessel Chikyu is the state-of-the-art scientific drill ship operated by the Japan Agency for Marine-Earth Science and Technology through the Center for Deep Earth Exploration for the Integrated Ocean Drilling Program. The NanTroSEIZE Stage 1 expeditions were implemented from September 2007 to February 2008. (Credit: Copyright: JAMSTEC/IODP)
Ads by Google
Advertise here
Blue Heron Bio GeneMaker
Gold standard gene synthesis Technology leader
www.blueheronbio.com/
Related Stories
Locations Of Strain, Slip Identified In Major Earthquake Fault (Feb. 27, 2009) — Deep-sea drilling into one of the most active earthquake zones on the planet is providing the first direct look at the geophysical fault properties underlying some of the world's largest earthquakes ... > read more
Core Samples From Subsea Fault System Off Japan Will Help Explain How Earthquakes Are Generated (Feb. 11, 2008) — Scientists aboard IODP scientific drilling vessel Chikyu collected 5,000 samples from the seismogenic zone known as the Nankai Trough. The samples will provide scientists with new sources of data and ... > read more
Deep-sea Drilling Yields Clues To Mega-earthquakes (Dec. 18, 2007) — Researchers fresh from an eight-week scientific drilling expedition off the Pacific coast of Japan have reported their discovery of strong variation in the tectonic stresses in a region notorious for ... > read more
Small Earthquakes are Useful Predictor of Large Ones (Dec. 5, 2007) — Conventional wisdom in seismology says slip on faults that rupture during the largest continental strike-slip earthquakes is generally limited to the seismogenic layer, the upper 15 km or so of the ... > read more
Deep-sea Scientific Drilling Program To Study Volatile Earthquake Zone Launched (Sep. 25, 2007) — Scientists begin exploring the origins of earthquakes at their source with the launch of the Nankai Trough Seismogenic Zone Experiment. On Sept. 21, the Japanese drilling vessel Chikyu departs from ... > read more
Search ScienceDaily
Number of stories in archives: 44,032
Find with keyword(s):
Enter a keyword or phrase to search ScienceDaily's archives for related news topics,
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Just In:
Why Sleep? To Boost Efficiency, Minimize Risk
Ultrathin LEDs: New Class Of Displays
Oxycholesterol: Greatest Heart Disease Risk?
Artificial Life One Step Closer?
New Way To Reproduce A Black Hole?
Aphids Saved From Gruesome Death By Virus
Human Appendix: No Biological 'Remnant'
Bioluminescent 'Green Bombers' From The Deep
Bioluminescent 'Green Bombers' From The Deep
Science Video News
Underwater Earthquakes
Seismologists investigating undersea earthquakes have found that molten rock lubricates faults. This decreases the amount of friction between sides. ... > full story
* Seismologists Find Large Earthquakes Can Trigger Smaller Ones In Unlikely Locations
* U.S.G.S., Caltech Seismologists Develop Online Tool to Predict Aftershocks
* Human Factors Researchers Develop Device To Measure Asthma Triggers
* more science videos
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