scholarly journals Extreme spatial and temporal variability of hydrothermal microbial mat communities along the Mariana Island Arc and southern Mariana back-arc system

2008 ◽  
Vol 113 (B8) ◽  
Author(s):  
Richard E. Davis ◽  
Craig L. Moyer
Keyword(s):  
Temporal Variability ◽  
Island Arc ◽  
Microbial Mat ◽  
Spatial And Temporal Variability ◽  
Back Arc ◽  
Mariana Island Arc

scholarly journals Spatial and temporal variability in a stratified hypersaline microbial mat community

2009 ◽  
Vol 68 (1) ◽  
pp. 46-58 ◽  
Author(s):  
Jesse G. Dillon ◽  
Scott Miller ◽  
Brad Bebout ◽  
Meredith Hullar ◽  
Nicolás Pinel ◽  
...  
Keyword(s):  
Temporal Variability ◽  
Microbial Mat ◽  
Spatial And Temporal Variability

scholarly journals Comparative geodynamics of Aleutian and Izu-Bonin-Mariana island-arc systems

2019 ◽  
pp. 27-43
Author(s):  
V. D. Chekhovich ◽  
A. N. Sukhov ◽  
M. V. Kononov ◽  
O. G. Sheremet
Keyword(s):  
North American ◽  
System Development ◽  
Island Arc ◽  
Aleutian Island ◽  
Main Role ◽  
The North ◽  
The Pacific ◽  
Lithospheric Plates ◽  
Back Arc ◽  
Mariana Island Arc

Fulfilled comparative analysis of the Aleutian and Izu-Bonin-Marian island-arc systems structure and geodynamic development. Izu-Bonin-Maian island-arc systems situated along сontinental margin of Eurasia in the West of Pacific Ocean. The Aleutian island-arc system is situated between the North American and Eurasian continents. Aleutian and Izu-Bonin-Marian island-arc systems appeared to be of the same age. Both island-arc systems form autonomous Philippine and Beringia small lithospheric plates. Izu-Bonin-Marianas island-arc system formed on exclusively geodynamic interaction of oceanic plate and back-arc basins, with the main role of the Pacific subduction. Aleutian system at the initial stage was formed as a result from separation of the part of Pacific Cretaceous crust by Aleutian subduction zone. The subsequent process of Aleutian system development was caused by geodynamics of movement of North American and Eurasian lithospheric plates. Pacific plate constant oblique subduction led to expansion of Aleutian island-arc system in the Western direction.

Volcanoes of the southwestern extension of the active Mariana island arc: New swath-mapping and geochemical studies

Island Arc ◽  
1998 ◽  
Vol 7 (3) ◽  
pp. 596-607
Author(s):  
F RYER ◽  
S UJIMOTO ◽  
S EKINE ◽  
J OHNSON ◽  
K ASAHARA ◽  
...  
Keyword(s):  
Island Arc ◽  
Swath Mapping ◽  
Geochemical Studies ◽  
Mariana Island Arc

Response of Corn Grain Yield to Spatial and Temporal Variability in Emergence

Crop Science ◽  
2004 ◽  
Vol 44 (3) ◽  
pp. 847 ◽  
Author(s):  
Weidong Liu ◽  
Matthijs Tollenaar ◽  
Greg Stewart ◽  
William Deen
Keyword(s):  
Grain Yield ◽  
Temporal Variability ◽  
Spatial And Temporal Variability ◽  
Corn Grain ◽  
Corn Grain Yield
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