ONR seafloor natural laboratories on slow‐ and fast‐spreading mid‐ocean ridges
Author(s) -
Tucholke Brian E.,
Macdonald Ken C.,
Fox Paul J.
Publication year - 1991
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1029/90eo00214
Subject(s) - seafloor spreading , ridge , geology , mid atlantic ridge , oceanic crust , mid ocean ridge , fracture zone , seismology , natural (archaeology) , igneous rock , crust , pacific ocean , oceanography , paleontology , subduction , tectonics
Long‐term Natural Laboratories for in‐depth studies of the seafloor at both a slowspreading (<30 mm/yr) and a fast‐spreading (>60 mm/yr) mid‐ocean ridge are being established by the Office of Naval Research. The two Natural Laboratories were selected for their representativeness of global mid‐ocean ridge environments, and for their logistic accessibility. The Natural Laboratory region for the slow‐spreading regime is on the Mid‐Atlantic Ridge from Kane Fracture Zone north to about 27°30″N (Figure 1), and the fast‐spreading counterpart is on the East Pacific Rise at about 8°–10°30″N, from Siqueiros to Clipperton Fracture Zone (Figure 2). Together, the two Natural Laboratories include most significant geologic variables that are thought to control both the shape and structure of the igneous crust and the scatter of acoustic wavefields from the bottom/subbottom (BSB) at low angles of incidence.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom