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Sunday, April 19, 2020 | History

4 edition of Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea found in the catalog.

Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea

Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea

Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal)

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Published by U.S. Dept. of the Interior, U.S. Geological Survey in [Reston, Va.?] .
Written in English

    Subjects:
  • Petroleum -- Geology -- Italy, Northern,
  • Petroleum -- Geology -- Adriatic Sea

  • Edition Notes

    Statementby Sandra J. Lindquist
    SeriesOpen-file report -- 99-50-M, U.S. Geological Survey open-file report -- 99-50-M
    ContributionsGeological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Pagination1 v
    ID Numbers
    Open LibraryOL13627611M
    OCLC/WorldCa45036757

    Rimini (/ ˈ r ɪ m ɪ n i / RIM-in-ee, Italian: (); Romagnol: Rémin; Latin: Ariminum) is a city in the Emilia-Romagna region of northern Italy and capital city of the Province of sprawls along the Adriatic Sea, on the coast between the rivers Marecchia (the ancient Ariminus) and Ausa (ancient Aprusa).It is one of the most notable seaside resorts in Europe with revenue from both Country: Italy. These slope-to-basin plays are prospective over large areas of the Adriatic Sea, mainly along the eastern margin of the Apulian platform, but also in areas farther to the east. Selected References Bertello, F., R. Fantoni, and R. Franciosi, , Overview of the Italy’s petroleum systems and related oil and gas occurrences: Conference and.


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Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea Download PDF EPUB FB2

The Porto Garibaldi total petroleum system dominates the Po Basin Province of onshore northern Italy and offshore Italy and Croatia in the northern Adriatic Sea. Porto Garibaldi contains Pliocene (primarily) and Pleistocene (secondarily) biogenic gas - approximately 16 TCP ( BBOE) ultimately recoverable - accumulated in co-eval siliciclasticCited by: The Porto Garibaldi total petroleum system dominates the Po Basin Province of onshore northern Italy and offshore Italy and Croatia in the northern Adriatic Sea.

Porto Garibaldi contains Pliocene (primarily) and Pleistocene (secondarily) biogenic gas – approximately 16 TCF ( BBOE) ultimately recoverable – accumulated in co-eval siliciclasticCited by: The Porto Garibaldi total petroleum system dominates the Po Basin Province of onshore northern Italy and offshore Italy and Croatia in the northern Adriatic Sea.

Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea [microform]: Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal) / by Sandra J.

Lindquist. Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea: Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal).

PETROLEUM OCCURRENCE AND CHARACTER There are fields in the Po Basin Province, with BBOE (48% produced) known, ultimately recoverable reserves (Petroconsultants, ) in three total petroleum systems. Ninety-seven percent of those ultimately recoverable reserves are in Italy; 3% are in Croatia.

This project aims at reconstructing the Late Messinian-Pleistocene 3D architecture and evolution of the Po Plain-Northern Adriatic foreland basin system (northern Italy).

Mesozoic petroleum system of the (northern Adriatic Sea and Po plain), the basin between the Trento and the Friuli platforms, here called the “northern Adriatic Basin,” possesses a Author: Roberto Fantoni. Lindquist, S.J.,Petroleum systems of the Po Basin province of northern Italy and the northern Adriatic Sea–Port Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal): U.S.

Geological Survey Open-File Report M, 19 p., 15 figs., 3 tables. During the Late Miocene–Pleistocene interval, a complex system of elongate foredeeps, the Po Plain-Adriatic Foredeep (PPAF), developed in the eastern sector of the Po Plain and in the northern Adriatic Sea, This system is the largest Late Miocene–Pleistocene complex of foredeep depocenters of the Periadriatic Basin with an overall length of km Cited by: The area falls within the Mesozoic thermogenic petroleum systems of central Adriatic Basin (Mattavelli et al., ).

The seep is located in the proximity of the Sarago field (Fig. 2), which. The Po Basin Province was part of the Adriatic microplate system developed between Africa and Europe. Early Mesozoic rocks record this breakup of Pangea – as well as an overall Mesozoic rising sea level – with pre-rift, Permo-Triassic continental siliciclastic rocks grading upward into Triassic rift sandstones, siltstones, shales.

The petroleum system of the oil and thermogenic gas fields of the Central and Southern areas of the Adriatic Sea is made from reservoir and source rocks of the Mesozoic carbonate succession. The offshore Adriatic Basin holds more than 50% of Italian gas reserves together with significant volumes of oil.

A number of large and giant-size biogenic gasfields and medium to large oilfields. Italy Petroleum Systems of the Po Basin Province of Northern Italy and the Northern Adriatic Sea: Porto Garibaldi (Biogenic), Meride/Riva di Solto (Thermal), and Marnoso Arenacea (Thermal).

In essence, the interval between the MIS 5e and the onset of the LGM (at ca. 26 ky BP) spanned a substantial shrinking of the Adriatic basin and the concurrent broadening of the Po plain drainage area with a stepwise displacement of the shoreline up to ca. km southeastward (Amorosi et al., ), and a relative position of sea level at ca Cited by: 1.

Introduction. The Northern Adriatic Sea has been recently studied in the framework of National and European projects aimed at evaluating its suitability for CO 2 geological storage, as part of the Carbon Capture and Storage (CCS) techniques, widely recognized as a key instrument for the reduction of the CO 2 emissions in the atmosphere.

CCS involves capturing the carbon dioxide produced by Cited by: 3. The petroleum exploration plays and the main structure of the Adriatic Sea. Most of the production of gas in Italy (about 10 billion m 3 per year), comes from the Northern Adriatic Sea.

These occurrences are associated with two important source rocks deposited in the foredeep terrigenous units of the foreland basins formed during the Cited by: Po ValleyEdit.

The vast valley around the Po is called the Po Basin or Po Valley (Italian Pianura Padana or Val Padana); in time it became the main industrial area of the country.

Inmore than 16 million people lived there, at the time nearly ⅓ of the population of y: Italy. Late Miocene–Middle Pleistocene sequences in the Po Plain – Northern Adriatic Sea (Italy): The stratigraphic record of modification phases affecting a complex foreland basin Manlio Ghielmi, Matteo Minervini, Claudio Nini, Sergio Rogledi, Massimo Rossi.

The Po Valley, Po Plain, Plain of the Po, or Padan Plain is a major geographical feature of Northern Italy. It extends approximately km in an east-west direction, with an area of 46, km2 including its Venetic extension not actually related to the Po river basin; it runs from the Western Alps to the Adriatic Sea.

The flatlands of Veneto and Friuli are often considered apart since they do not drain into the Po. Lindquist, S.J.,Petroleum systems of the Po Basin province of northern Italy and the northern Adriatic Sea: Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal): U.S.

Geological Survey Open-File Report M, 19 p., 15 figs., 3 tables. Petroleum Systems of the Po Basin Province of Northern Italy and Po Basin mixed forests | DOPA Explorer Study area: (a) River Po basin (m DTM) and flood-plain mapping.

M Petroleum Systems of the Po Basin Province of Northern Italy and the Northern Adriatic Sea: Porto Garibaldi (Biogenic), Meride/Riva di Solto (Thermal), and Marnoso Arenacea (Thermal) -N South and North Barents Triassic-Jurassic Total Petroleum System of the Russian Offshore Arctic.

These gas and oil reserves are part of the Po basin Province of Northern Italy and the Northern Mediterranean Sea.

[] In the s, investigation works aimed at discovering gas and oil reserves in the Middle and Southern Adriatic basins intensified, and by the decade's end, oil and natural gas reserves were discovered southeast of the Bari, Brindisi—Rovesti and Giove oil nates: 43°N 15°E / 43°N 15°ECoordinates:.

We describe the Miocene petroleum system in the context of the geology of the Northern Apennines as a system fed by multiple sources including some potential for deep oil accumulation.

The presence of sources deeper than the Miocene reservoir is required by the high thermal maturity of the oils, the thermogenic nature of methane and the high Cited by: Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal).

South and North Barents Triassic-Jurassic total petroleum system of the Russian offshore Arctic [microf The Red Sea Basin Province, Sudr-Nubia(!) and Maqna(!) petroleum systems [microform] / by Sandra J. Lind Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea [microform].

petroleum systems of the Po basin and the adjoining Northern Apennines and its comparison with the data on Petroleum Systems of the South Caspian basin of Azerbaijan, allow one to conclude that there are many common features of the basins as: sub-oceanic earth crust was generated during the Jurassic (Paleo Tethys ocean).

Petroleum systems and play maturity •The Adriatic basin belongs to genetically related Ionian and Apulian geological domains in Italy and Albania where one order of magnitude higher number of exploration wells exists with a significant amount of discovered oil and gas fields.

Hydrocarbon occurrences in Italy derive from a variety of petroleum systems which are the result of a complex geological history (Bertello et al, ).

Oil fields are present in the Mesozoic carbonate in Po Plain, Adriatic Sea, Southern Apennines and Sicily. The Adriatic Abyssal Plain, more commonly referred to as the Adriatic Basin, is an oceanic basin under the Adriatic Adriatic Sea's average depth is metres ( ft), and its maximum depth is 1, metres (4, ft); however, the North Adriatic basin rarely exceeds a depth of metres ( ft).

Petroleum systems of the Po Basin Province of northern Italy and the northern Adriatic Sea Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal) Lindquist, Sandra J.

This paper presents a preliminary study of the water profile with reference to microbiological parameters, required by Directive /07/EC (European Community ) concerning the management of bathing water quality, in the coastal belt of the Province of Venice (Italy, Northern Adriatic Sea).

A historical database has been implemented with monitoring data for the period Cited by: 6. Petroleum Systems of the Po Basin Province of Northern Italy and the Northern Adriatic Sea: Porto Garibaldi (Biogenic), Meride/Riva Di Solto (Thermal), and Marnoso-Arenacea (Thermal) Lindquist, S.J.

Pre-orogenic tectonics in the Umbria-Marche sector of the Afro-Adriatic continental margin. The broad Po-Veneto plain and the Northern Adriatic include Italy's most important gas province and the country's largest oil field discovered so far, Villa Fortuna-Trecate ().

Petroleum Systems and Mixed Oil in the Barents Sea and Northern Timan-Pechora Basin, Russia* Meng He1, Kenneth E. Peters2, J. Michael Moldowan3, and Alla Rovenskaya4 Search and Discovery Article # () Posted Septem They form reservoirs for light oil, gas, and condensate fields in the Emilian and Romagna nappes along the southern edge of the Tertiary Po basin of northern Italy.

Petroleum systems of the Po Basin province of northern Italy and the northern Adriatic Sea: Porto Garibaldi (biogenic), Meride/Riva di Solto (thermal), and Marnoso Arenacea (thermal) Lindquist, S.J.

Locating and quantifying geological uncertainty in three-dimensional models: analysis of the Gippsland Basin, southeastern Australia. [8] Strong seasonal variability dominates the northern Adriatic Sea. The passing of synoptic midlatitude events, Figure 1.

Geography and bathymetry of the northern Adriatic Sea. Shown in detail is the northern Adriatic Sea as defined by the m isobath.

Wind stations at Trieste, Venice, Acqua Alta and Pula are depicted with a by:. Lombardy (/ ˈ l ɒ m b ər d i, ˈ l ʌ m-/ LOM-bər-dee, LUM-; Italian: Lombardia [lombarˈdiːa]; Lombard: Lombardia, Western Lombard: [lũbarˈdiːa], or Lombardéa, Eastern Lombard: [lombarˈde.a]) is one of the twenty administrative regions of Italy, in the northwest of the country, with an area of 23, square kilometres (9, sq mi).

About 10 million people live in Lombardy, forming Capital: Milan.The Italian Peninsula, also known as Italic Peninsula or Apennine Peninsula, is a peninsula extending from the southern Alps in the north to the central Mediterranean Sea in the south.

It is nicknamed lo Stivale (the Boot). Three smaller peninsulas contribute to this characteristic shape, namely Calabria (the "toe"), Salento (the "heel") and Gargano (the "spur").The Adriatic Sea is a body of water separating the Italian Peninsula from the Balkan Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Italy, Montenegro and Slovenia.