ce Proceedings of the Asiatic Society of Bengal. [N.S., XV, 
On the Inclination of the thrust-plane or reversed fault 
between the Siwalik and Murree zones of formations, 
near Kotli, Jammu province.—By C. §. MrppLEemtss. 
ibes, jis reference to data phi from geological details laid 
dines ci on ma w 1”=1 mile contoured sheets by the Surve ey of India, the 
accurate angle ‘of inclination of the above, gett: which is widely different 
from what poe generally been assumed in similar Sub-Himalayan sections 
elsewhere 
The succession of the tertiary marine faunas in the Eas 
Indies, based principally on a ie 4 fog ihenbaeata: 
tous gastropods.—By E. VREDENB 
A detailed analysis of the oe tae aoe enter the lower 
eocene of the Ranikot of Sind, the upper limit of which corresponds with 
the Cuisian. It is equally — ‘that the Khirther ris the equivalent of 
the Lutecian. tercalation of a well-developed stage, locally termed 
the Laki, indicates that th ian seque i additional 
ter issing, or imperfectly developed, in the classical exposures of th 
Anglo- Parisian ° 8s are given for consider equivalent 
to Le F nnian”’ of the Paris basin, and to the Lybian of Egypt 
This stage appears to be w loped in the Mediterranean countries 
where it has been mistaken sometimes for the lowe ce e 
fo utecian. The B e of —- is upper. eocene and 
ng 
ari fauna coincides largely, on the one hand, with the oligocene 
fauna of Europe, on the other a with that of the Yenangyaung — 
(amended) of Burma, whose oligocene pb is t — reby established. In 
= way has been sis lished the low ocen he Gj 
a 
ries ava. 
of the ‘* — miocene”’ (mainly vindobonian) Tjilanang series 0 
a dia. Mekran and Kari a faunas of India 
closely uae with the pliocene Sonde series of Jav 
Py 
| 
ae 
5 
~ 
5 
Two new fossil localities in the tertiary rocks of the Garo 
Hills —By E. 8. Prnroip 
The fossil ne described are on the southern borders of the Garo 
Hills; the first is four miles north of Dalu on the road to Tura and the 
second is i 
ts 
ous bed in the two localities is of the same age. The absence of similar 
beds from the intervening sections examined m may be due to the poor state 
of exposure—most a te the area in ‘which the rocks might be aapected to 
occur is under alluvi 
The rock containing the a is a blue shale cone _ inpincccug rd 
hard bands. The fossiliferous eps n both localiti not more 
two feet in thickness a in eac tote single se pa “ext om 
observed. This was crowded seg —- ca preserved shells, chiefly gas- 
tropods and lamellibranche, The horizon is near the top of the sandstone 
mulitic li = 
8. pre 
ing dip is nontete and the occurrence of the fossiliferous bed at the 
—- ra Pete’ of the hills indicates a position amongst the highest rocks 
ae Hi 
redenburg, who has kindly undertaken to examine eth fossils, 
reports ‘that there is every reason to conclude that the rock in w t 
temporaneous with the Gaj of Western India ite there- 
