Bathymetry and Crustal Thickness Variations from Gravity Inversion and Flexural Isostasy

Author(s):  
Carla Braitenberg ◽  
Elena Pagot ◽  
Yong Wang ◽  
Jian Fang
2021 ◽  
Vol 9 ◽  
Author(s):  
Liang Zhang ◽  
Xiwu Luan

The Okinawa Trough (OT) is an incipient back-arc basin, but its crustal nature is still controversial. Gravity inversion along with sediment and lithospheric mantle density modeling are used to map the regional Moho depth and crustal thickness variations of the OT and its adjacent areas. The gravity inversion result shows that the crustal thicknesses are 17–22 km at the northern OT, 11–19 km at the central OT, and 7–19 km at the southern OT. Because of the crust with a thickness larger than 17 km, the slow southward arc movement, and scarce contemporaneous volcanisms, the northern OT should be in the stage of early back-arc extension. All of the moderate crustal thickness, high heat flow, and intense volcanism at the central OT indicate that this region is probably in the transitional stage from the back-arc rifting to the oceanic spreading. A crust that is only 7 km thick, lithosphere strength as low as the mid-ocean ridge, and MORB-similar basalts at the southern OT demonstrate that the southern OT is at the early stage of seafloor spreading.


Geology ◽  
2000 ◽  
Vol 28 (4) ◽  
pp. 303-306
Author(s):  
Jennifer L. Lewis ◽  
Steven M. Day ◽  
Harold Magistrale ◽  
Jennifer Eakins ◽  
Frank Vernon

2019 ◽  
Vol 20 (7) ◽  
pp. 3225-3247 ◽  
Author(s):  
Nina Lebedeva‐Ivanova ◽  
Carmen Gaina ◽  
Alexander Minakov ◽  
Sergey Kashubin

2004 ◽  
Vol 228 (3-4) ◽  
pp. 267-280 ◽  
Author(s):  
Céline Tirel ◽  
Frédéric Gueydan ◽  
Christel Tiberi ◽  
Jean-Pierre Brun

Author(s):  
Lupei Zhu ◽  
Brian J. Mitchell ◽  
Nihal Akyol ◽  
Ibrahim Cemen ◽  
Kivanc Kekovali

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