Zobrazeno 1 - 10
of 19
pro vyhledávání: '"T. Ricchiuto"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 97, Iss 3-4 (2017)
The stratigraphic and paleogeographic analysis of the Carnian-Norian boundary succession in central Lombardy allows the recognition of a new unit, the Castro Formation. This unit, 100-250 m thick, is represented by carbonatic intraformational breccia
Externí odkaz:
https://doaj.org/article/a2a0fadf4dc24ae9a3681405eb62f859
Publikováno v:
Environmental Pollution. 129:321-330
Single-well reactive tracer tests, such as the push-pull test are useful tools for characterising in-situ bioattenuation processes in contaminated aquifers. However, the analytical models that are used to interpret push-pull data may be over-simplifi
Publikováno v:
Chemical Geology. 106:429-440
The abundance and isotopic composition of He, Ne and Ar have been determined in 19 gas samples taken from the Dosso degli Angeli hydrocarbon gas field, between 3000- and 3750-m depth in the Po Basin. Carbon isotope ratios in these samples vary betwee
Publikováno v:
Earth and Planetary Science Letters. 109:493-504
A mud breccia has been repeatedly cored from four mud diapir fields located on the crest of the Mediterranean Ridge. This breccia is composed of subrounded clasts supported by a clay-rich matrix and ranges in age from Cretaceous to early Miocene. Sed
Autor:
E. Pavanel, T. Ricchiuto
Publikováno v:
59th EAGE Conference & Exhibition.
Publikováno v:
Organic Geochemistry. 10:391-400
The crude oils of the Po Basin are characterized by means of different analytical techniques (capillary GC of the saturated and aromatic hydrocarbons, carbon isotopic composition of the fractions, capillary GC/MS of the steranes and terpanes, V and N
Autor:
Martin Schoell, T. Ricchiuto
Publikováno v:
Organic Geochemistry. 13:311-318
Pliocene reservoirs in the Apulian Basin in south Italy produce gases of highly variable composition. C 2+ concentrations range between 0 and 8%, nitrogen between 0 and 20%, CO 2 between 0 and 80%, and δ 13 C and δD in methane between -67 and -41%
Publikováno v:
Geological Society, London, Special Publications. 12:227-227
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