Extinct spreading center
WebThe extinct spreading center is associated with a short-wavelength (λ 40 km) free air gravity anomaly low of 10–20 mGal and a region of rough acoustic basement. We infer that the Coral Sea basin began opening at about 62 m.y. B.P. at a half-spreading rate of 2.4 cm/yr and that spreading ceased at about 56 m.y. B.P. WebJun 8, 2024 · The extinct spreading center (gray) as defined by Christeson et al. (2014). Orange, yellow, and green lines mark previous limit of oceanic crust (LOC) interpretations (Pindell and Kennan, 2009; Hudec et al., 2013; Christeson et al., 2014), while white rectangles mark the LOC interpreted in the GUMBO seismic-refraction data. …
Extinct spreading center
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WebDec 28, 2024 · We explore a well-known extinct spreading center within the South China Sea. Using ocean bottom seismometers and the receiver function technique, we determine the thickness of the magmatic crust, and a parameter (Vp/Vs) that reflects the structure of the underlying crust. We find that, approaching the extinct spreading axis, the crust ... WebFeb 10, 1995 · The Labrador Sea contains a rare example of an abandoned mid-ocean ridge where active accretion of oceanic crust ceased due to a change in the spreading …
WebFeb 1, 1995 · The aseismic ridge system of the South China Sea, extinct since about 17 Ma, subducts below the central part of the Taiwan-Luzon volcanic arc, North Luzon … WebSep 3, 2024 · According to Sasaki et al. ( 2014 ), the West Philippine Spreading Center (WPSC) was probably active 28 Ma, with a half-spreading rate of 60 mm/year; however, previous studies have reported slower spreading rates of 18 mm/year (Lewis and Hayes, 1980; Hilde and Lee 1984; Jonas et al. 1991 ).
WebAug 26, 2014 · The extinct spreading center of the Huatung Basin is located near the southernmost Ryukyu subduction zone. Furthermore, it shows a strong plate coupling between the overriding and subducting plates (Hsu 2001) in the same area. Seismic hazard analysis and evaluation is needed for the southernmost Ryukyu subduction zone area. WebFeb 9, 2024 · An extinct, late Jurassic-to-earliest Cretaceous ridge-and-fracture zone geometry in the western Gulf of Mexico (GOM), and extinct seafloor ridge segments in the eastern Gulf of Mexico (EGOM), were previously identified using the vertical gradient of satellite-derived free-air gravity data.
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WebDec 1, 1999 · Abstract. The Central Basin fault in the center of the West Philippine Basin was first discovered ∼50 yr ago. It is a 1000-km-long ridge oriented northwest to … carabine à verrou browningWebDec 1, 2024 · This paper explores the evolutional process of back-arc basin (BAB) magma system at final spreading stage of extinct BAB, Shikoku Basin (Philippine Sea) and assesses its tectonic evolution... carabine browning auto nouveautéWebMay 26, 2015 · Delescluse et al. (2015) identified an OCC at the extinct ultraslow Labrador Sea spreading center using tomographic imaging, where serpentinized mantle velocities were observed beneath just... carabine express drilling eric mathelonWebJan 20, 2024 · The extinct spreading center (ESC), denoted as ESR (extinct spreading ridge) by Eddy et al. (2014), is marked by a pronounced trough in basement. Blue and black lines show the depths from refraction to basement and Moho respectively. brizo shower flangeWebTrough is an extinct spreading center, but that result was controversial due to limited data coverage [e.g., Small and Abbott, 1998]. Subsequent ship track studies [Billen and Stock, 2000], however, showed that the trough has mor-phology typical of extinct spreading ridges. The Osbourn paleospreading center formed when a large oceanic plateau carabine express beretta silverWebSep 1, 1996 · Abstract We present a joint analysis of seismic reflection and refraction profiles across an extinct spreading center in the Labrador Sea. The refraction data are used to constrain the crustal and subcrustal velocity structure, and the deep multichannel reflection data are used to determine the nature of the tectonic fabric within the crust. brizo shower handlesWebMar 1, 1980 · An OBS (ocean-bottom seismograph) airgun refraction survey was conducted near the extinct spreading center in the 18–21 m.y. old Shikoku Basin, North Philippine Sea. The P-wave velocity structure of the ocean crust (layers IIA and IIB) is in accord with that of the average ocean crust. P to S converted waves were remarkably well recorded … carabine feinwerkbau p700 occasion