Jan 12, 2002· ABSTRACT Many types of carbonate platforms have been described, from homoclinal ramps to rimmed shelves and a full spectrum of variations in between; the distinction between these different types can be problematic. Nevertheless, classification of carbonate platforms is not just a semantic or academic issue. For example, it is clearly important for the accurate interpretation of …
Christie-Blick, N. and K.T. Biddle 1985 Deformation and basin formation along strike-slip faults. In: N. Christie-Blick and K.T. Biddle (eds): Strike-slip deformation, basin formation and sedimentation–Soc. Econ. Paleont. Spec. Pub. 42: 1–34 CrossRef Google Scholar
AKOME, K. and HARAGUCHI, M. (1963): Geology and ore deposits of the Toyoha mine. Mining Geol., 13, 93-99 (in Japanese with English abstract). AKOME, K. and HARAGUCHI, M. (1967): The characteristics of fracture and mineralization of the Toyoha mine.
May 01, 2009· The Phuket Group is the oldest rock unit in the Phuket-Takua Pa-Krabi region of the Thai Peninsula. The Group comprises two Formations: a Lower Formation of Ordovician, or possibly Cambrian, to Lower Permian age, exceeding 3 km in thickness, and an Upper Formation of early Permian age between 100 and 200m thick.
Summary. The characteristic pattern of the subsidence, deformation, uplift and erosion of foreland basins, or exogeosynclines, has long been recognized by geologists as an integral part of the geosynclinal cycle yet only descriptive models have been proposed.
Along the Jurassic-Cretaceous dolomitic beds of the Tripolis Unit in the Mainalon Mt. and the surrounding areas, products of a widespread breccias have been recognized. This brecciation extended through at least two stages, early- and late diagenetic, respectively.
Dec 01, 1992· An up-dated data base is a matter of importance and urgency in order for encouraging a process-oriented approach to the study of reef evolution. The evolution of reefs is a major section of a Priority Program of the Deutsche Forschungsgemeinschaft devoted to ‘Global and regional controls of biogenic sedimentation’. Biological, paleontological and geological approaches in the study of ...
Jan 01, 1991· It is widely observed that joint spacing is proportional to bed thickness in sedimentary rocks. The origin of this proportionality is explored by observation of joint spacing in the Monterey Formation of California and by one-dimensional numerical …
Henry William Posamentier (born December 4, 1948) is an American geologist.He helped pioneer and develop the modern approach to sequence stratigraphy, blending the disciplines of sedimentology, stratigraphy, and depositional systems analysis, largely within the context of oil and gas exploration.During the past decade he pioneered and popularized the discipline of seismic …
Jun 28, 2005· Soc Econ Paleont Miner Spec Publ, pp 203–231 Google Scholar Dullo W-Chr (1980) Paleontology, facies, and geochemistry of the Dachstein Limestone (Upper Triassic) in the southwestern Gesäuse Mountains, Styria, Austria. Facies 2:55–122 Google Scholar Dullo W-Chr, Lein R (1982) Facies environment of the Lechkogelbeds (Carnian, Alps).
The effects of Ag +, Al 3+, and Cr 3+ ions on calcium carbonate polymorphs were investigated using a double diffusion technique. The experimental results, analyzed by the equivalency rule, were as follows: (i) Ag +, Al 3+, and Cr 3+ ions promoted the formation of aragonite; (ii) in the presence of Ag + ions, Ag 2 CO 3 crystals acted as a nucleus for the epitaxial growth of aragonite; (iii) Al ...
San Cassiano Formation (Anisian-Carnian) is a geologic formation located on the Southern Alps (Northeast of Italy) in the Dolomites.These Triassic dolomites are considered to be a classic example of ancient carbonate platforms. As the allochthonous elements in the Shale strata (Cipit boulders) show a good preservation, fossils and microbialites contained in these elements are useful in ...
Along the Jurassic-Cretaceous dolomitic beds of the Tripolis Unit in the Mainalon Mt. and the surrounding areas, products of a widespread breccias have been recognized. This brecciation extended through at least two stages, early- and late diagenetic, respectively. The first brecciation stage is considered to have taken place penecontemporaneously or soon after the deposition related with ...
Free Web tutorials sequence stratigraphy, tutorials carbonate petrology, seismic interpretation sequence stratigraphy exercises Lower Cretaceous South Africa, seismic interpretation sequence stratigraphy exercises Bahamas Miocene, seismic interpretation sequence stratigraphy exercises Lower Cretaceous Alaska, clastic outcrop interpretation sequence stratigraphy exercises of Bookcliffs ...
88 SOUTHERN CALIFORNI ACADEMA OY F SCIENCES MIOCENE PF burrows are assigned to Thalassinoides on the basis of comparison to illustrations in Ekdal ee t al. (1984 figs., 3-5 15-5), . Ichnofacies According to Ekdale et al. (1984), firm but uncemented substrate ars e associated
Riv. It. Paleont. Strat., 94/3: 425-454. BERSEZIO R. & FORNACIARI M. (1988) - Tectonic framework of the Lombardy foothills (Southern Alps) between Brianza and Lake Iseo. Rend. Soc. Geol. It., 11: 75-78. BERTOTTI G. (1990) - The deep structure of the Monte Generoso basin: an extensional basin in the south-Alpine Mesozoic passive continental ...
Above the Plio-Pleistocene siliciclastic basement, five seismic units, Unit 1 to Unit 5 in descending order, were identified and correlated to the Pleistocene Ryukyu Group and Holocene sediments. A major tectonic event between ca. 1.7 Ma and 1.2 Ma deformed the Plio-Pleistocene siliciclastic basement (Unit 6).
The Middle Oxfordian strata in the southern part of the Cracow-Wielun Upland consist of platy and bedded limestones (‘normal facies’), of massive limestones as well as locally of mass flow sediments. Massive limestones, prevailing in the Upper Oxfordian, form commonly carbonate buildups, which are made up predominantly of cyanobacterial allochems and to a minor amount of siliceous sponges.
Summary. The concept of a quiet, nearly motionless, and certainly currentless deep-sea floor lacking the processes of erosion so prevalent in shallower seas was well ingrained in scientific thought until discoveries of the past decade revised this serene and static picture.