RESEARCH IN CHINA. 









Li-kuan-ts’u 
me 7 

. 
sandstone 
iS) 
2 oy) 

& 
PLATE XVI 

grahite 
dolerite, 
yn tie 
marble 
poophyry 
marble in 
SQporphyry 

0° marble 
conglomerate 
25°quartzite 


in sandstone 
SS 
é iS 
x porphyry dikes 
sandstone 

AS 
Yung-li-chong 
sandetone 
be 3° 
4 ae 
‘ > }*-Ts’au-kcia-tien 
3 
CoN 
sandstone 
Yen-kia-tién 
or 
3 
eS 
st? ? 
flat 
vonglomerate in sandstone 
S 
*) as 
porphyry dike: 
‘ Wang-kia-ling 
6 Wa-fang-k’ou 

sandstone 
aw AWS 
f 20° 
= Ny sandstone 
3 
oY dolerite dike 
— Se 
overthrust . \ era brown grit 
S 
Z hs \ 
2° green limestone 
25° 
shales Pe 25° 
[] Fu-chou 
randy 25 
flat (8 
© 
/ ~S\randy— 
Hf 2 \tat~ white quartzite 
MSIE ; 
3 
Ss over shale 



& Ir-shi-li-p’u 
sandy flat 
( /olive earthy limestone 
alluvial flat 
7 +e 
5 Ma-tien-tzi 
Pie 
Yt? 
Woive sandstone 
ay 
{E102 purple and green shale 
V4 green shale 
ZW, (green shale 
$72 olive sandstone 
ae it 
m y -* olive limestone 
Wu-kia-tien 
A449 
Huang-kia-chuang 
| overthrust 
purple shales\, . 
gray quartzite 
J 45°/ 
7 
gneiss 
Ping-tun 

sandy flat) San-kuatmiau 
Soillof green yale and 

oul imestoaoe > 
! Pu-lan-tien 
\ —— =~) b Leh 
9 Wa-fang-tién 
POATES, ENGR’G CO., N.Y. 
ie2e 
10 Miles 

10 
20 Kilometers 

LIAU-TUNG. 
