最終更新日：2022/12/24
From the evidence of the latest Ludlovian to Early Devonian ophiolite, which crops out from the northern slope of Mt. Saarming to Kümüx and areas further east (Wang Zuoxun et al., 1986, 1990; Xiao Xuchang et al., 1990), the South Tianshan back-arc basin had already developed into a finite ocean basin along the Hantengri-Kümüx Fault after the Ludlovian.
編集履歴（0）
元となった例文
From
the
evidence
of
the
latest
Ludlovian
to
Early
Devonian
ophiolite,
which
crops
out
from
the
northern
slope
of
Mt.
Saarming
to
Kümüx
and
areas
further
east
(Wang
Zuoxun
et
al.,
1986,
1990;
Xiao
Xuchang
et
al.,
1990),
the
South
Tianshan
back-arc
basin
had
already
developed
into
a
finite
ocean
basin
along
the
Hantengri-Kümüx
Fault
after
the
Ludlovian.
