40Ar/39Ar mineral ages from the Southern Cape Breton Highlands and Creignish Hills, Cape Breton Island, Canada: evidence for a polyphase tecnothermal evolution

MLA

Dallmeyer, R.David, and J.Duncan Keppie. “40Ar/39Ar Mineral Ages from the Southern Cape Breton Highlands and Creignish Hills, Cape Breton Island, Canada: Evidence for a Polyphase Tecnothermal Evolution.” Journal of Geology, vol. v101, no. n4, July 1993, p. 467. EBSCOhost, widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsggo&AN=edsgcl.14169433&authtype=sso&custid=ns315887.

APA

Dallmeyer, R. D., & Keppie, J. D. (1993). 40Ar/39Ar mineral ages from the Southern Cape Breton Highlands and Creignish Hills, Cape Breton Island, Canada: evidence for a polyphase tecnothermal evolution. Journal of Geology, v101(n4), 467.

Chicago

Dallmeyer, R. David, and J. Duncan Keppie. 1993. “40Ar/39Ar Mineral Ages from the Southern Cape Breton Highlands and Creignish Hills, Cape Breton Island, Canada: Evidence for a Polyphase Tecnothermal Evolution.” Journal of Geology v101 (n4): 467. http://widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsggo&AN=edsgcl.14169433&authtype=sso&custid=ns315887.