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SC Finney - Ordovician of the World, 2011 - books.google.com
... 857-3" I '" © Instituto Geologico y Minero de Espana 2011 11 I505 GSSP BOUNDARY INTERVALS
ARE CRITICAL FOR CHARACTERIZATION ... instances, its encompassing series and system must
be correlative as widely as possible geographically and between facies and with ...
D Gao - Geophysics, 2011 - geophysics.geoscienceworld.org
... Gao, 2007) have shown that textural homogeneity, contrast, and randomness are effective in
identifying and classifying critical seismic facies, such as channel sand, levee, overbank, mass
transport complex, marine shale, and salt in deep-marine depositional systems (Figure 5 ...
Cited by 1 - Related articles - All 3 versions
[PDF] from open.ac.ukJ Chambers, R Parrish, T Argles, N Harris… - Tectonics, 2011 - oro.open.ac.uk
... It is therefore evident that the timing, duration and kinematics of slip on these faults forms a critical
test of the aforementioned models for Himalayan orogenesis. ... kinematic history [Yin, 2006; Webb
et al., 2007]. Amphibolite-granulite facies (generally migmatitic ...
Cited by 1 - Related articles - All 5 versions
II Likhanov, VV Reverdatto, PS Kozlov… - Doklady Earth …, 2011 - Springer
... isograd) in the absence of cordierite. The critical assemblage Ky + St + Grt + Ms +
Bt + Qtz + Pl + Sil (fine fibrolite) with andalusite relics was formed under conditions
of the kyanite schist facies. These rocks comprise a 4 to 5 ...
Related articles - All 3 versions
W LI, A DONOVAN, S STAERKER… - 2011 GSA Annual …, 2011 - gsa.confex.com
... structural units. The differences in production are, to a large extent, controlled by
facies changes, and understanding the heterogeneity and lateral facies variability
within the Eagle Ford, thus, is critical for future drilling success. ...
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