Results 1 to 10 of about 11,816 (290)
A new species of <i>Galathea</i> (Decapoda, Galatheidae) from the seamounts of the Easter Island area (Southeast Pacific Ocean Ridge) associated with a sea urchin. [PDF]
ZookeysGallardo Salamanca MLÁ +2 more
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Decoding microbial diversity, biogeochemical functions, and interaction potentials in red sea hydrothermal vents. [PDF]
Environ MicrobiomeAltalhi S +10 more
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Continental slivers in oceanic transform faults controlled by rift inheritance
Balázs A, Gerya T, Tari G.
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, 2017 Mid-ocean ridges illustrate well how volcanic, tectonic, hydrothermal and sedimentary processes sculpt geomorphology in the deep ocean. Because of their poor accessibility (lying 2700 m below sea level on average) and remote locations, the development and deployment of new technology has been important for the discovery and investigation of new ...
Mitchell, Neil; id_orcid
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Some of the next articles are maybe not open access.
Scientific American, 1990
The Mid-Ocean Ridge girdles the earth like the seam of a baseball. For more than 75,000 kilometers, this submerged range of razorback mountains--many higher than the greatest peaks on land--marks the restless boundary between continental plates. An analysis of this huge structure reveals a fascinating picture of how it is created by magma welling up as
Kenneth C. Macdonald, Paul J. Fox
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The Mid-Ocean Ridge girdles the earth like the seam of a baseball. For more than 75,000 kilometers, this submerged range of razorback mountains--many higher than the greatest peaks on land--marks the restless boundary between continental plates. An analysis of this huge structure reveals a fascinating picture of how it is created by magma welling up as
Kenneth C. Macdonald, Paul J. Fox
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2010
Mid-ocean ridges are the oceanic counterparts of continental graben structures. Both are zones of extension although mid-ocean ridges have substantially higher spreading rates and also mark plate boundaries where new oceanic crust and lithosphere are formed.
Wolfgang Frisch +2 more
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Mid-ocean ridges are the oceanic counterparts of continental graben structures. Both are zones of extension although mid-ocean ridges have substantially higher spreading rates and also mark plate boundaries where new oceanic crust and lithosphere are formed.
Wolfgang Frisch +2 more
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2004
Two thirds of our planet are covered by ocean, beneath which stretches basaltic oceanic crust. The eruptions that produce this crust are hidden from direct observation. Remote sensing instruments with which to record the countless volcanic eruptions that occur under the ocean waves each year are few and far between. Even the fact that mid-ocean ridges (
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Two thirds of our planet are covered by ocean, beneath which stretches basaltic oceanic crust. The eruptions that produce this crust are hidden from direct observation. Remote sensing instruments with which to record the countless volcanic eruptions that occur under the ocean waves each year are few and far between. Even the fact that mid-ocean ridges (
openaire +2 more sources
2007
A map of the ocean basins (Fig. 5.1) shows that their most conspicuous topographic feature is the system of mid-oceanic ridges, the crests of which rise on average 1000–3000 m above the adjacent ocean floor. Such ridges extend through all the major ocean basins, with a total length in excess of 60 000 km.
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A map of the ocean basins (Fig. 5.1) shows that their most conspicuous topographic feature is the system of mid-oceanic ridges, the crests of which rise on average 1000–3000 m above the adjacent ocean floor. Such ridges extend through all the major ocean basins, with a total length in excess of 60 000 km.
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1999
Preface J. R. Cann, H. Elderfield and A. Laughton 1. Sensitivity of teleseismic body waves to mineral texture and melt in the mantle beneath a mid-ocean ridge Donna K. Blackman and J.-Michael Kendall 2. Evidence for accumulated melt beneath the slow-spreading Mid-Atlantic Ridge M. C. Sinha, D. A. Navin, L. M. Mac Gregor, S. Constable, C.
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Preface J. R. Cann, H. Elderfield and A. Laughton 1. Sensitivity of teleseismic body waves to mineral texture and melt in the mantle beneath a mid-ocean ridge Donna K. Blackman and J.-Michael Kendall 2. Evidence for accumulated melt beneath the slow-spreading Mid-Atlantic Ridge M. C. Sinha, D. A. Navin, L. M. Mac Gregor, S. Constable, C.
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Nature, 1967
THE Mid-Oceanic Ridge, a broad fractured arch more than 40,000 miles long, is the largest tectonic feature on the surface of the Earth. Associated with the centre of the ridge over much of its length is an axial fracture or rift which is the locus of shallow earthquakes.
G. LEONARD JOHNSON, BRUCE C. HEEZEN
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THE Mid-Oceanic Ridge, a broad fractured arch more than 40,000 miles long, is the largest tectonic feature on the surface of the Earth. Associated with the centre of the ridge over much of its length is an axial fracture or rift which is the locus of shallow earthquakes.
G. LEONARD JOHNSON, BRUCE C. HEEZEN
openaire +1 more source