The Erlian Basin is located in the Central Asia-Mongolian fold belt between
the Siberian and Sino-Korean Cratons. It is a Mesozoic continental rift ba
sin composed of 52 individual fault-depressions. The main phase of rifting
took place during the Early Cretaceous when a series of fluvial-lacustrine
sediments were deposited. Each depression forms an independent sedimentary
system and behaves as an independent petroleum system. Hydrocarbon source r
ocks are found in the upper Arshan and lower Tengger Formations. These are
mainly type II source rocks and are mainly located in oil generation 'windo
w' at the present day. A series of oilfields and commercial oil hows have b
een found in the basin, highlighting its good petroleum potential. Many of
these oils are heavy.
Six oil samples from the Anan and ten from the Jirgalangtu Depressions have
been subjected to routine geochemical analytical techniques in order to ev
aluate the origins. The methods used include gas chromatography of the satu
rated and aromatic hydrocarbon fractions, gas-chromatography-mass-spectrome
try of the saturated hydrocarbon fraction and stable carbon isotope analyse
s. The trace metal elements of the biodegraded oils from the Jirgalangtu De
pression were also analysed by atomic absorption spectroscopy.
Two types of heavy oils: primary and biodegraded were identified on the bas
is of these data. The former includes both immature and mature heavy oils.
A 'filtering-and-spill' process was proposed to explain the origin of prima
ry mature heavy oils (or tar-mat) in the Anan Depression. The biodegraded o
ils from the Jirgalangtu Depression were ranked and classified in terms of
the degree of biodegradation, using a series of geochemical parameters base
d on the gas chromatographic concentrations and biomarker fingerprints of g
as-chromatography-mass-spectrometry of the saturated hydrocarbon fraction.
The relationship between oil saturation and porosity indicates that the hea
vy oils in the Jirgalangtu Depression were biodegraded after they accumulat
ed. (C) 1998 Elsevier Science Ltd. All rights reserved.