Extensive normal faulting during exhumation revealed by the spatial variation of phengite K-Ar ages in the Sambagawa metamorphic rocks, central Shikoku, SW Japan

Island Arc ◽  
2015 ◽  
Vol 24 (2) ◽  
pp. 245-262 ◽  
Author(s):  
Toru Takeshita ◽  
Koshi Yagi ◽  
Chitaro Gouzu ◽  
Hironobu Hyodo ◽  
Tetsumaru Itaya
1965 ◽  
Vol S7-VII (5) ◽  
pp. 787-821 ◽  
Author(s):  
Jean Aubouin ◽  
Jean Dercourt

Abstract The oldest rocks exposed on Crete (Greece) are Paleozoic? metamorphic rocks. Five series are represented in the overlying sedimentary cover, whose deposition took place in a geosynclinal environment from Triassic to Eocene time. Molasse deposits are the principal representatives of the late geosynclinal phase (Miocene); marls and limy sandstones and conglomerates were formed during the postgeosynclinal phase (Pliocene). Major faults are the dominant tectonic feature of the island. Two nappes are identified: the Pindus nappe on which the ophiolitic (sub-Pelagonian) nappe is superimposed in places. Differential uplift and intense normal faulting have broken the island into a number of massifs separated by lowlands.


2019 ◽  
Vol 125 (6) ◽  
pp. 447-452
Author(s):  
Koki Nakata ◽  
Nao Kusuhashi ◽  
Satoshi Saito ◽  
Hiroaki Ohfuji ◽  
Masakazu Nara

2021 ◽  
Vol 144 ◽  
pp. 104256
Author(s):  
Jiameng Zuo ◽  
Zhonghai Wu ◽  
Guanghao Ha ◽  
Mengmeng Hu ◽  
Chunjing Zhou ◽  
...  

2012 ◽  
Vol 118 (Supplement) ◽  
pp. S79-S89 ◽  
Author(s):  
Tetsuo Kawakami ◽  
Yoshiharu Nishioka
Keyword(s):  

1989 ◽  
Vol 84 (12) ◽  
pp. 429-443 ◽  
Author(s):  
NORIE FUJIBAYASHI ◽  
TAKASHI NAGAO ◽  
HIROO KAGAMI ◽  
MASATOSHI IWATA ◽  
KOICHI TAZAKI

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