Predicting
Physicochemical Properties of Upper Jurassic Circum-Arctic Crude Oil
Peters, Kenneth E.1, L. Scott
Ramos2, John E. Zumberge3, Zenon
C. Valin1, Donald L. Gautier4 (1) U.S. Geological Survey,
Menlo Park, CA (2) Infometrix, Inc, Bothell, WA (3) GeoMark Research, Inc, Houston, TX (4) U. S. Geological
Survey, Menlo Park, CA
Biomarkers (molecular fossils) and stable
carbon isotope ratios were measured for >550 crude oil samples expelled from
Upper Jurassic source rock collected from wells and seeps north of ~55oN
latitude. A unique, multi-tiered chemometric
(multivariate statistical) decision tree was used to classify genetically
distinct Upper Jurassic oil families from West Siberia, the North Sea, and offshore Labrador. The method, which we
call decision-tree chemometrics, utilizes PCA
(principal components analysis), multiple tiers of KNN (K-Nearest Neighbor),
and SIMCA (soft independent modeling of class analogy) models to classify and
assign confidence limits for newly acquired oil samples and source-rock
extracts. Geochemical data for each oil sample were also used to infer the type
of organic matter input, lithology, and depositional
environment of each organofacies of the source rock.
Partial least squares analysis (PLS) of the measured geochemical data was used
to predict various physicochemical properties of the samples, such as API
gravity, sulfur, and metal content. Present-day and paleogeographic
maps predict the distribution of physicochemical properties of oil expelled
from different organofacies of the Upper Jurassic
source rock. For example, families of oil samples in West Siberia show concentric
distributions that mimic the measured physicochemical properties and are
controlled by oxic-anoxic and terrigenous-marine
conditions during deposition of the Bazhenov
Formation source rock.