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[PDF][PDF] An overview of the Izu-Bonin-Mariana subduction factory
The lzu-Bonin-Mariana (IBM) arc system extends 2800km from near Tokyo, Japan to Guam
and is an outstanding example of an intraoceanic convergent margin (IOCM). Inputs from …
and is an outstanding example of an intraoceanic convergent margin (IOCM). Inputs from …
The late Mesozoic–Cenozoic tectonic evolution of the South China Sea: A petrologic perspective
This paper presents a review of available petrological, geochonological and geochemical
data for late Mesozoic to Recent igneous rocks in the South China Sea (SCS) and adjacent …
data for late Mesozoic to Recent igneous rocks in the South China Sea (SCS) and adjacent …
Hafnium isotope evidence for 'conservative'element mobility during subduction zone processes
The high field strength elements (HFSE) play a critical role in the interpretation of chemical
variation within subduction-related magmas by providing an assumed mantle-dominated …
variation within subduction-related magmas by providing an assumed mantle-dominated …
[PDF][PDF] Origin of back‐arc basin magmas: Trace element and isotope perspectives
The compositions of back-arc basin basalts (BABB) can usefully be viewed as products of
four factors:(1) the composition of inflowing mantle and its preconditioning during flow to the …
four factors:(1) the composition of inflowing mantle and its preconditioning during flow to the …
Geochemical and Sr‐Nd isotopic characteristics of volcanic rocks from the Okinawa Trough and Ryukyu Arc: Implications for the evolution of a young, intracontinental …
R Shinjo, SL Chung, Y Kato… - Journal of Geophysical …, 1999 - Wiley Online Library
The Okinawa Trough is an incipient intracontinental back arc basin that has developed
behind the Ryukyu arc‐trench system. To explore its magmatic evolution and the nature of …
behind the Ryukyu arc‐trench system. To explore its magmatic evolution and the nature of …
Hf-Nd element and isotope perspective on the nature and provenance of mantle and subduction components in Western Pacific arc-basin systems
This paper develops methods for using the integrated study of Hf-Nd element and isotope
covariations to define the nature and provenance of the mantle and subduction inputs to …
covariations to define the nature and provenance of the mantle and subduction inputs to …
Geochemical and Nd–Pb isotopic characteristics of the Tethyan asthenosphere: implications for the origin of the Indian Ocean mantle domain
It is unclear why the Pb, Nd, and Sr isotopic composition of the modern mid-ocean ridge
basalts (MORB) from the Indian Ocean is different from that of the North Atlantic and Pacific …
basalts (MORB) from the Indian Ocean is different from that of the North Atlantic and Pacific …
Magma genesis in the New Britain island arc: further insights into melting and mass transfer processes
Quaternary volcanic rocks from the New Britain island arc display a wide range in chemical
compositions. The source of the lavas shares isotopic characteristics with Indian Ocean type …
compositions. The source of the lavas shares isotopic characteristics with Indian Ocean type …
Tracing the Indian Ocean mantle domain through time: isotopic results from old West Indian, East Tethyan, and South Pacific seafloor
The isotopic difference between modern Indian Ocean and Pacific or North Atlantic Ocean
ridge mantle (eg variably lower 206Pb/204Pb for a given εNd and 208Pb/204Pb) could …
ridge mantle (eg variably lower 206Pb/204Pb for a given εNd and 208Pb/204Pb) could …
Geochemical evolution within the Tonga–Kermadec–Lau arc–back-arc systems: the role of varying mantle wedge composition in space and time
New trace element and Sr, Nd, and Pb isotope data for lavas from the active Tonga–
Kermadec arc in the southwest Pacific, the volcano of Niua fo'ou in the back-arc Lau Basin …
Kermadec arc in the southwest Pacific, the volcano of Niua fo'ou in the back-arc Lau Basin …