Investor Presentaiton
LEMIGAS
TECTONIC SETTING
INTRODUCTION
VICINI
THAILAND
W7/38
M-1
MYANMAR
THAILAND
MERGUI RIDGE
WEST MERGUI
B-BASIN
SUB-BASI
CENTRAL
EAST MERGUI
SUB-BASIN
W9/38
W8/38
SHELF
W1/38
W2
MERGUT
W3/38
THAILAND
KHLONG MARUI FAULT
W4/38
W5/38
NORTH SUMATRA
BASIN
MALACCA
PLATFORM
W6/38
THAILAND
MALAYSIA
PM1
ARUN HIGH
PEUSANGAN
MOUNTAIN
BARISAN
SUMATRA
SUMATRAN FAULT SYSTEM
96°00'
UST FRONT
ARCH
ASAHAN
6200
480
Andreason, et. Al., 1997
The Mergui - North Sumatera
basin is bounded by
convergence of Mergui Ridge
with continental crust of Sunda
Craton to the north, Asahan
Arch to the east, Barisan
Mountain to the south, and the
Mergui ridge to the west.
The main tectonic elements
dominated by relatively N-S
and NW-SE trending highs and
deeps
These highs and deeps divide
the larger basin into several
sub-basins
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