In Geological Society of America, Abstracts with Programs, vol. 35, no. 3, p. 15.
HIGH-RESOLUTION CLIMATIC AND TECTONIC FRAMEWORK FOR THE TRIASSIC-JURASSIC
RIFTS OF EASTERN NORTH AMERICA AND MOROCCO AND THE DISTRIBUTION OF POTENTIAL
SOURCE ROCKS
OLSEN, Paul E., Lamont-Doherty Earth Observatory, Columbia Univ, 61
RT 9W, Palisades, NY 10964-1000, polsen@ldeo.columbia.edu, KENT, Dennis V.,
Geological Sciences, Rutgers Univ. and Lamont-Doherty Earth Observatory,
Piscataway, NJ 08854, and ET-TOUHAMI, Mohammed, LGVBS, Département
des Sciences de la Terre, Université Mohamed Premier, Oujda, Oujda,
60 000, Morocco
With the advent of the Newark basin astronomically calibrated paleomagnetic
time scale, it has become at least in principle possible to correlate other
sections globally at a much higher degree of precision than possible with
most biostratigraphic data. Within the last few years, this possibility has
been at least partially realized in North America and Morocco with large
portions of the polarity stratigraphy of several basins (spread over a 10°
paleolatitudinal latitudinal swath) being worked out and correlated with
the Newark basin time scale. In addition a more limited polarity sequence
has been worked out in Greenland at about 30° paleolatitude. These correlations
demonstrate a strong correspondence between sedimentary facies and latitudinal
position as well as with their position within presumed extensional pulses,
the stratigraphic consequence of which are the tectonostratigraphic sequences
that subdivide the basin sections (TS I – IV).
In eastern North America, significant potential source rocks are restricted
to lacustrine strata deposited in very low latitude basins for the Triassic
in the early phases of TS-II and TS-III and over a broader latitudinal swath
in the Early Jurassic in the early phases of TS-IV. Deposits formed in higher,
but still tropical latitudes, include eolian sands, making potentially excellent
reservoirs, and evaporites making excellent potential seals and traps (TS-III
and TS IV). Good potential source rocks are present in the lacustrine latest
Triassic and Early Jurassic of Greenland, deposited in more temperate latitudes.
The temporospacial matrix using these paleolatitude and climatic data make
predictions about the stratigraphic and structural location of facies important
to the hydrocarbon system. For example, good source rocks are most likely
to be present in the buried South Georgia rift, relatively high in TS III
for climatic reasons, but these are likely to be gas prone, because the tectonic
milieu would favor shallow lakes and coals. Similarly, the only real chance
for significant source rocks in the Argana and Fundy basins would be in the
deeper and buried parts of the basins in the lower half of TS-II and TS-IV.