The Qinling orogen preserves a record of la
te mid-Pro
terozoic
to Cenozoic
tec
tonism in cen
tral China. High-pressure me
tamorphism and ophioli
te emplacemen
t (Songshugou ophioli
te) assembled
the
Yang
tze cra
ton, including
the lower Qinling uni
t, in
to Rodinia during
the
ter border=0 SRC=/images/glyphs/BQ1.GIF>1.0 Ga Grenvillian orogeny. The lower Qinling uni
t then rif
ted from
the Yang
tze cra
ton a
t ter border=0 SRC=/images/glyphs/BQ1.GIF>0.7 Ga. Subsequen
t in
tra-oceanic arc forma
tion a
t ter border=0 SRC=/images/glyphs/BQ1.GIF>470–490 Ma was followed by accre
tion of
the lower Qinling uni
t firs
t to
the in
tra-oceanic arc and
then
to
the Sino-Korea cra
ton. Subduc
tion
then imprin
ted a
ter border=0 SRC=/images/glyphs/BQ1.GIF>400 Ma Andean-
type magma
tic arc on
to all uni
ts nor
th of
the nor
thern Liuling uni
t. Oblique subduc
tion crea
ted Silurian–Devonian WNW-
trending, sinis
tral
transpressive wrench zones (e.g., Lo-Nan, Shang-Dan), and La
te Permian–Early Triassic subduc
tion reac
tiva
ted
them in dex
tral
transpression (Lo-Nan, Shang-Xiang, Shang-Dan) and subduc
ted
the nor
thern edge of
the Yang
tze cra
ton. Exhuma
tion of
the cra
tonal edge formed
the Wudang me
tamorphic core complex during dominan
tly pure shear crus
tal ex
tension a
t ter border=0 SRC=/images/glyphs/BQ1.GIF>230–235 Ma. Pos
t-collisional sou
th-direc
ted shor
tening con
tinued
through
the Early Jurassic. Cre
taceous reac
tiva
tion of
the Qinling orogen s
tar
ted wi
th NW–SE sinis
tral
trans
tension, coeval wi
th large-scale Early Cre
taceous crus
tal ex
tension and sinis
tral
trans
tension in
the nor
thern Dabie Shan; i
t presumably resul
ted from
the combined effec
ts of
the Siberia–Mongolia&
mdash;Sino-Korean and Lhasa–Wes
t Burma&
mdash;Qiang
tang–Indochina collisions and Pacific subduc
tion. Regional dex
tral wrenching was ac
tive wi
thin a NE–SW ex
tensional regime be
tween
ter border=0 SRC=/images/glyphs/BQ1.GIF>60 and 100 Ma. An Early Cre
taceous Andean-
type con
tinen
tal magma
tic arc, wi
th widespread Early Cre
taceous magma
tism and back-arc ex
tension, was overprin
ted by shor
tening rela
ted
to
the collision of Yang
tze–Indochina Block wi
th
the Wes
t Philippines Block. S
trike–slip and normal faul
ts associa
ted wi
th Eocene half-graben basins record Paleogene NNE–SSW con
trac
tion and WNW–ESE ex
tension. The Neogene(?) is charac
terized by normal faul
ts and NNE-
trending sub-horizon
tal ex
tension. Pleis
tocene(?)–Qua
ternary NW–SE ex
tension and NE–SW con
trac
tion comprises sinis
tral s
trike–slip faul
ts and is par
t of
the NW–SE ex
tension imposed across eas
tern Asia by
the India–Asia collision.