Arc evolution and continental crust formation at the Izu–Bonin–Mariana arc system

2006 ◽  
Vol 70 (18) ◽  
pp. A638 ◽  
Author(s):  
Y. Tatsumi ◽  
N. Takahashi ◽  
S. Kodaira ◽  
Y. Kaneda
2015 ◽  
Vol 424 ◽  
pp. 84-94 ◽  
Author(s):  
Kenichiro Tani ◽  
Daniel J. Dunkley ◽  
Qing Chang ◽  
Alexander R.L. Nichols ◽  
Hiroshi Shukuno ◽  
...  

Geology ◽  
2016 ◽  
Vol 44 (10) ◽  
pp. 819-822 ◽  
Author(s):  
Hélène Delavault ◽  
Bruno Dhuime ◽  
Chris J. Hawkesworth ◽  
Peter A. Cawood ◽  
Horst Marschall ◽  
...  

Author(s):  
A. L. Dergachev

Tectonic evolution of the Earth is a principle global factor responsible for uneven distribution of lead and zinc reserves in geological time. Cyclic changes in productivity of lead-zinc ore-formation processes resulted from periodical amalgamation of most blocks of continental crust, formation, stabilization and final break-up of supercontinents. Many features of age spectrums of lead and zinc reserves are caused by gradual increase of volume of continental crust resulting from accretion of island arcs to ancient cratons, widening of distribution of ensialic environments of ore-formation and increasing role of continental crust in magmatic processes.


Science ◽  
1978 ◽  
Vol 200 (4345) ◽  
pp. 1003-1011 ◽  
Author(s):  
M. T. McCulloch ◽  
G. J. Wasserburg

Island Arc ◽  
1998 ◽  
Vol 7 (3) ◽  
pp. 395-407 ◽  
Author(s):  
A SAHIKO T AIRA ◽  
S ANEATSU S AITO ◽  
K AN A OIKE ◽  
S UMITO M ORITA ◽  
H IDEKAZU T OKUYAMA ◽  
...  

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