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Italian cross section (recent)
Western U.S. cross section (370 Ma)
87Sr/86Sr = 0.706
hingeline
Burchfiel & Royden(1991)
Royden & Burchfiel (1991)Lund (2008)Lund (2008) BurchfielRoydenAntler_Overheads.ppt
Draw two cross sections on theother side of this page, oneacross the region of modernItaly, the other across westernU.S. at ~370 Ma (during theAntler orogeny).List some of the majorsimilarities and differences. Onthe western U.S. cross section,show the topographic divide.The following passage is inBurchfiel and Royden:
Explain briefly why each of these is important, andinclude these ideas in your cross section.
Following Burchfiel nd Royden, sketch the position of the Klamath-Sierran volcanic arc,Havallah Basin, Antler allochthon and Antler foredeep at an initial stage of development, andat a late stage of development. Show where extension is occurring, sediment transport(arrows going from source to sink), and the topographic divide. (Basin and Range extension has widened the area between the hingeline and the rift margin. Draw your sketch on the map shown, which is of the current locations.)
Antler Orogeny (again)
hing
e-lin
e
East
ern
Med
iterra
nean
Sea
, with
Aeg
ean
Sea
betw
een
Turk
ey a
nd G
reec
e.Th
e Ae
gean
is h
ighl
y ex
tend
ed c
ontin
enta
l cru
st p
ulle
d ap
art a
s th
e H
elle
nic
subd
uctio
n re
treat
s to
the
sout
h.Vo
lcan
ic a
rc (r
ed-fi
lled
circ
les)
lie
with
in th
e ex
tend
ed A
egea
n Se
a.C
rete
is p
art o
f the
topo
grap
hic
divi
de b
etw
een
thru
st b
elt t
o th
e so
uth
and
the
Aege
an to
the
north
.