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        | Field Trip | 
       
      
        We plan to have a field excursion on September 29th 2018, that
         offers opportunities to observe topographical and geological features accompanied 
         by fault activities along the Median Tectonic Line (MTL), the most prominent and 
         long-lived active fault system in Japan, traced back to Cretaceous times. The MTL 
         bounds the Ryoke high-temperature metamorphic belt overlain by sediments of the 
         Late Cretaceous Izumi Super-group and the Sanbagawa high-pressure metamorphic belt. 
         In the morning, we will observe geomorphological manifestation of the EW-trending 
         MTL fault system at the middle reaches of the Yoshinogawa river. A lunch break will 
         be offered at Oboke gorge, the heartland of the Sanbagawa metamorphic belt, followed 
         by a river boat riding during which we will observe geological structures related 
         to the exhumation of the high-pressure rocks.
        
        
        Excursion course: 
        07:30 Leaving the hotel for Stop 1 
        09:30 Stop 1: Fault scarp at Ikeda (MTL geomorphology) 
        11:00 Leaving Stop 1 for Oboke 
        11:40 Lunch at Oboke Roadside Station 
        Stop 2: River Boat riding at Oboke gorge
        13:30 Leaving Oboke for the Tokushima airport and Kobe 
        15:30 Arriving at the Tokushima airport 
        17:15 Arriving at the Sannomiya station 
        17:30 Arriving at the Shin-Kobe station 
        
         
        Stop 1: Ikeda fault, a branch of the MTL fault system.
        Ikeda, Miyoshi city, Tokushima prefecture (N34°01’44”, E133°48’04”)
        
        
         
        
        
        
         
        
        
        Note: Participants who requested to join the field trip by July 31 have been approved. 
         
       
        
        
        
      
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