@article{185, author = {R. von Huene and G. Keller}, title = {Cenozoic migration of Alaskan terranes indicated by paleontologic study}, abstract = {
Comparison s o f microfossils fro m deep-sea cores, fro m sample s o f an explorator y drill hole, and fro m dredged rocks o f the Gulf o f Alaska, with coeval microfossil assemblage s on the Nort h America n continent, provide constraints on the northwar d migratio n o f the Yakuta t block and the Princ e William terran e during Tertiary time. The estimated paleolatitudes of microfauna and flora indicate that: (1 ) the Prince William terran e wa s attache d to North Americ a in its present position by middl e Eocen e time (40 to 42 Ma) , consistent with models derived fro m paleomagneti c data , and (2) the adjacent Yakuta t block was 30 {\textpm} 5 {\textdegree} south o f its present position in earl y Eocen e (50 Ma) , 20 {\textpm} 5 {\textdegree} south in middl e Eocen e (40 to 44 Ma) , and 15 {\textpm} 5 {\textdegree} south in lat e Eocen e tim e (37 to 40 Ma) , thus requiring a northwar d motion o f about 30 {\textdegree} since 50 Ma . Moreover , the Yakuta t block wa s at least 10{\textdegree} south o f the Princ e William terran e during Eocen e time . Thes e dat a ar e consistent with migratio n o f the Yakuta t block with the Pacifi c and Kul a plate s for a t least the last 50 Ma . T h e collision o f the Yakuta t block with Nort h Americ a resulted in subduction o f the block coincident with uplift o f the Kena i Mountains. Th e extension o f the Kena i Mountains into the Kodiak are a suggests tha t a southwest extension o f the Yakuta t block collided with the Kodiak margi n and was completely subducted. Th e subducted extension o f the Yakuta t block could have connected the now subducting head o f Zodiak deep-sea fan to a Nort h America n sourc e o f sediment during deposition o f the fan.\ PDF
}, year = {1985}, journal = {AAPG Special Publication}, pages = {121-136}, url = {http://archives.datapages.com/data/circ_pac/1/121_b.htm}, language = {eng}, }