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Post Info TOPIC: Giant drill ship


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JOIDES Resolution
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Geoscientists Drill Deepest Hole in Ocean Crust in Scientific Ocean Drilling History

For eight weeks beginning in November 2009, off the coast of New Zealand, an international team of 34 scientists and 92 support staff and crew on board the scientific drilling vessel JOIDES Resolution (JR) were at work investigating sea-level change in a region called the Canterbury Basin. It proved to be a record-breaking trip for the research team.
From November 4, 2009 to January 4, 2010, the IODP research team drilled four sites in the seafloor. One site marked the deepest hole drilled by the JR on the continental shelf (1,030 metres), and another was the deepest hole drilled on a single expedition in the history of scientific ocean drilling (1,927 metres).
Another record was broken for the deepest sample taken by scientific ocean drilling for microbiological studies (1,925 metres).

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RE: Giant drill ship
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Researchers on Chikyu Report Successful Riser-Drilling
Kumano Basin off Kii Peninsula, approximately 58 km southeast of Japan - Despite harsh weather and ocean conditions, and complex geological characteristics of its drill site, the deep-sea drilling vessel CHIKYU, for the first time in the history of scientific ocean drilling, conducted riser-drilling operations to successfully drill down to a depth of 1,603.7 metres beneath the sea floor (at water depth of 2,054 metres).

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Nankai Trough Seismogenic Zone Experiment
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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 and tsunamis.
The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is the first geologic study of the underwater subduction zone faults that give rise to the massive earthquakes known to seismologists as mega-thrust earthquakes.

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RE: Giant drill ship
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A Japanese research vessel carrying the world's largest deep-sea drill has completed its first expedition after collecting data it hopes will help discover more about earthquakes, officials said Saturday.
The 210-metre ship Chikyu - the Japanese word for "Earth" - was on a mission to clarify the causes of earthquakes and uncover the secrets of climate change.
Chikyu on Thursday completed its first 56-day assignment in the Nankai Trough, a Pacific Ocean zone between two major tectonic plates that has produced powerful, destructive earthquakes off southwest Japan over the past 1 500 years, according to the Japan Agency for Marine-Earth Science and Technology, which developed the ¥57-billion vessel.

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exp314-014_s.jpg
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Credit  JAMSTEC

 The Chikyu is headed to the Nankai Trough

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One of the most ambitious earth science expeditions yet mounted to gain a better understanding of the earthquake process, has begun off the coast of Japan, involving geologists from the universities of Southampton and Leicester.
Dr Lisa McNeill, of the University of Southampton's School of Ocean and Earth Science, based at the National Oceanography Centre, Southampton, and Joanne Tudge, of the Department of Geology, University of Leicester, are taking part in the multi-disciplinary study of a 'subduction' zone off the Japanese coast, aboard the deep-sea drilling vessel Chikyu (which means 'Planet Earth' in Japanese). This is the maiden scientific voyage of this vessel, which has unique capabilities enabling it to access new regions of the Earth's crust.
Large-scale subduction earthquakes are the world's most powerful seismic events and the cause of major catastrophes, such as the 2004 earthquake and tsunami in the Indian Ocean.
Japan, which has endured devastating earthquakes in cities such as Kobe in 1995, has made major investments in technology, including Chikyu, to learn more about seismic activity near its shores.
Lisa McNeill, a lecturer at Southampton, joins the Nankai Trough Seismogenic Zone Experiment (or NanTroSEIZE) expedition, part of the Integrated Ocean Drilling Program (IODP), as a scientific participant, but will also serve as a co-chief scientist on a later phase of the experiment in 2009.
PhD student Joanne Tudge is part of the Geophysics and Borehole Research Group in the Department of Geology at Leicester, which has a long-standing history of providing logging services and expertise for the IODP. Her research focuses on interpreting data from the borehole to better understand the sediments. On this NanTroSEIZE expedition she will be working to classify the rocks and understand the physical properties of the sediments in the subduction zone.
The project is ambitious in scale - the first phase alone is the longest period of scientific ocean drilling ever attempted in one area. In the second phase, colleagues will attempt to break the scientific ocean drilling depth record by targeting a fault around 3500m below the sea floor.
During the third phase, the drill ship aims to reach the main plate boundary at 6km and place long-term monitoring tools. The experiment will take samples and install observatories to assess, for example, how strain is building up on the fault, the effects of fluid on rocks and the physical properties of sediments as they are deformed.

'The scale of this experiment is unprecedented and I am very excited to be taking part. This is an extremely challenging expedition but the results should give us a much greater understanding of the processes responsible for generating earthquakes and tsunami' - Dr Lisa McNeill.

The project (Nankai Trough Seismogenic Zone Experiments or NanTroSEIZE) is supported by the Integrated Ocean Drilling Program (IODP), a marine research initiative jointly funded by Japan, the United States, a consortium of European countries, the People's Republic of China, and South Korea. The Natural Environment Research Council (NERC) provides the UK's contribution to the IODP through ECORD (the European Consortium for Ocean Research Drilling).
NanTroSEIZE, and the inaugural expedition which has just begun, is led by chief project scientists Dr Harold Tobin, a marine geologist on the faculty of University of Wisconsin-Madison, and Dr Masa Kino****a, a marine geophysicist at the Japan Agency for Marine-Earth Science and Technology (JAMSTEC), a leading research institution in Japan.

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Borehole Map
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The GE Scientific Borehole map has been improved. Now, in addition to viewing the location of all holes drilled during DSDP, ODP, and IODP, web users can select links to newly digitised online expedition publications that correspond to drill sites.  Proposed drill sites also have been updated and linked to the IODP Site Survey Data Bank.

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Deep Corer
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The deeper you can sample the seafloor, the further back in time you can go
Since the early part of the 20th century, scientists have been going to sea on ships equipped with long, hollow pipes called corers. These corers are used to collect seafloor sediments, plunging into the ocean bottom and capturing long stratified plugs of the seabed. These sediments contain clues to a myriad of past conditions and events in the Earths oceans and climate.
Over decades, technology and methods for handling coring systems have become safer, and core samples have become longer, reaching 20 to 25 metres  in length. This longer reach provides access to deeper, older sediments, and thus a look further back into Earth history.
In the 1970s, Charlie Hollister at the Woods Hole Oceanographic Institution (WHOI) recovered an historic core from the Northeast Pacific. It contained one of the longest continuous records of ocean basin history: 65 million yearsback to times when dinosaurs still roamed the planet. As scientists still do today, Hollister and colleagues studied tiny fossilised shells and fish teeth found in the core. Careful analysis of these remnants can reveal the temperature, water chemistry, and other characteristics of ancient oceans.

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Nankai Trough Seismogenic Zone Experiment
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It promises to be one of the grand scientific challenges of this decade.
Researchers are about to drill down into an earthquake zone at the Nankai Trough off the coast of Japan.
The project, which will cost hundreds of millions of dollars over the next 10 years, is being coordinated by the Integrated Ocean Drilling Programme.
It seeks to understand the causes of deadly quakes and tsunami by pulling up cores for study and by putting down sensors to monitor changes in the rock.
The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) expects to get under way in September.

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Earth's oceanic crust
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Researchers report that an approach used for years to understand the structure of Earth's oceanic crust is flawed and geoscientists will have reconsider the correspondence between seismic data and rock units when mapping formations of young oceanic crust.
The new finding alters the view of how new crust is formed at mid-ocean ridges, how heat and chemicals flow through oceanic crust and how life can exist in the hot, inhospitable environment deep below the seafloor.

Scientists Gail Christeson and Kirk McIntosh from the Institute for Geophysics at The University of Texas at Austin’s Jackson School of Geosciences, and Jeffrey Karson from Syracuse University, publish their findings in this week's edition of Nature. Their research reveals that seismic data, widely used by geoscientists to create a picture of the geology below the seafloor, cannot reliably map the boundaries between rock units in young oceanic crust. Despite this limitation, seismic data may hold keys to understanding how fluids reside and circulate through the crust and the limits of the subsurface biosphere.

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