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| style="background: #FED85D" | Eocene

file:St58OverviewFG32.JPG|{{figure number|8}}Cuba. 50 Ma: top lower Eocene.<ref name=Pardo_2009 /> file:St58OverviewFG33.JPG|{{figure number|9}}Cuba. 40 Ma: base upper Eocene.<ref name=Pardo_2009 />

...cording the eastward migration of the [[Caribbean plate]] since the late [[Eocene]]. ...(28-99 mi) wide, of intensely folded and faulted Middle Jurassic to middle Eocene rocks consisting, from north to south, of:

...l determinations in the upper [[Cenozoic]]. Nonmarine diatoms range from [[Eocene]] to Holocene and also are useful in the upper [[Cenozoic]]. These microfos

...16 giant oil fields. [[Reservoir rock]]s range in age from Precambrian to Eocene. The Upper Cretaceous Sirt [[Shale]] is the major source rock. It represent ...oduction]] in the El Bouri oil field of the Tripolitania Basin is from the Eocene nummulitic limestone, producing 60,000 bbl/d with 800 million barrels of re

* [[Eocene]]

...7>Wright, J. D., and K. G. Miller, 1993, Southern Ocean influences on late Eocene to Miocene deep-water circulation: American Geophysical Union Antarctic Res ...Permian, Jurassic, Late Cretaceous, and several intervals within the Late Eocene to [[Holocene]]), the strontium curve can be used as a chronometer because

...oading, continued salt-ridge growth, and eventual rupture of the overlying Eocene chalk along the ridge crest. Salt, squeezed out of the ridge, localized int ...uth Pass 62 field. Salt rises from a depth of approximately 8000 m through Eocene chalk and Miocene, Pliocene, and Pleistocene clastics to within 200 m of th

...an, Y. Lu, H. Liu, Y. Hao, Z. Xie, L. Peng, X. Du, and H. Hu, 2017, Middle Eocene paleohydrology of the Dongying Depression in eastern China from sedimentolo ...2019. Shale oil resource potential and oil mobility characteristics of the Eocene-Oligocene Shahejie Formation, Jiyang Super-Depression, Bohai Bay Basin of C

| Lower [[Tertiary]] (centered on [[Eocene]], ~50-40 Ma)

...f these deposits. The most important oil-shale deposits are those of the [[Eocene]] [[Green River Formation]] in the states of Colorado, Utah, and Wyoming in

...c and paleoenvironmental variables across a condensed section in the Upper Eocene at St. Stephens Quarry, Alabama. Copyright: Loutit et al.;<ref name=ch17r60 ...ama. The condensed section corresponds to the unnamed blue clay. Overlying Eocene [[Red Bluff]] and [[Bumpnose Formation]]s are [[Sea_level_cycle_phase_and_s

...Bay field]], charged during the Late Cretaceous and tilted during the late Eocene<ref name=ch11r1>Atkinson, C., McGowen, J., Block, S., Lundell, L., Trumbly,

...ssic), Germav Formation (Late Cretaceous-Paleocene), and Gercüş Formation (Eocene) units. These asphaltites were developed in NE-SW striking fractures that w ...may have started from the end of the Early Cretaceous to Paleocene and the Eocene time. They sometimes enter the oil window up to the end of the Miocene time

| Norton Basin, Alaska || High || [[Eocene]]/[[Paleocene]] || Direct || Smith<ref name=Smith_1994>Smith, J. T., 1994, | Taranaki Basin, New Zealand || High || Eocene || Direct ||

The Zala basin consists of various Eocene fault blocks, unconformably overlain by a Middle and Upper Miocene section

...mbli Formation anywhere in the basin, indicating that the overlying late [[Eocene]] Akli Formation is the topmost regional seal to the petroleum system acros ...Thumbli Formation]] where [[basement]]-related faults propagate into the [[Eocene]] section.

...nce for source potential for [[crude oil]] in the upper Paleocene to lower Eocene Wilcox Formation. If lower Tertiary Wilcox equivalent or uppermost Jurassic

...Formation of Albian age and the upper part of the Pabdeh Formation (Middle Eocene to Oligocene). A third source rock was developed locally and is known as th ...il expulsion from the Diyab source rock likely began toward the end of the Eocene.<ref name=Gumati_1993>Gumati, Y. D., 1993, [http://www.sciencedirect.com/sc

| 12 || 34 || Bai Hassan || Jeribe/Kirkuk Group/Jaddala || Miocene-Oligocene-Eocene || Carbonate || Fatha || Evaporite || | 30 || 32 || Kirkuk || Pila Spi/Avanah/Jaddala || Late-Middle Eocene || Carbonate || Fatha || Evaporite || "Main Limestone"

# The Tethyan Himalayan Sequence (THS), mainly [[Proterozoic]] to [[Eocene]] sediments. deformed in an [[Paleogene]] [[fold]]-thrust belt.<ref name=":

...arbon source potential of organic facies of the lacustrine Elko Formation (Eocene/Oligocene), northeast Nevada, in J. Woodward, F. F. Meissner, and J. L. Cla ...ral extracts from two distinct facies within the nonmarine Elko Formation (Eocene/Oligocene) of Nevada. The lignitic siltstones are dominated by terrestrial

...lomite (Ca_1.12Mg_0.88(CO₂)₂) of Eocene age. The prominent modulated structure is typical of sedimentary dolomite,

...MR), Pakistan. (D) Algal laminations containing dolomite and evaporites in Eocene Chorgali Formation, KMR, Pakistan. (from Awais et al., 2020b)]] ...b; Lucia, 2004; Martín-Martín et al., 2015; Kordi et al., 2017). In Middle Eocene Avon Park Formation (South Florida, USA), dolomitization (cementation) redu

...nd to the top Cretaceous, the polygonal faults, and the [[Paleocene]] to [[Eocene]] faults that do not connect to the deeper faults. ...]n (Ostanin et al., 2012<ref name=Ostaninetal2012a />). The Paleocene to [[Eocene]] transition is characterized by an angular [[unconformity]], on top of whi

...revised Paleogene geochronology, in D. R. Prothero, W. A. Berggren, eds., Eocene-Oligocene Climatic and Biotic Evolution: Princeton, Princeton University Pr

| Norton Basin, Alaska || High || [[Eocene]]/[[Paleocene]] || Direct || Smith<ref name=Smith_1994>Smith, J. T., 1994, | Taranaki Basin, New Zealand || High || Eocene || Direct ||

...rt et al., 2001<ref name=Konertetal2001 />). From the [[Permian]] to the [[Eocene]], the area was a broad stable passive margin where the deposition of mainl

...xygenated waters. Examples include the lacustrine Green River oil shale of Eocene age in Wyoming, Colorado, and Utah; and the marine Galena oil rock of Ordov

...ref> In Syria, the main Paleozoic, Triassic, Jurassic and upper Cretaceous/Eocene source-rocks which have fed the Palmyrides, Euphrates and NW corner hydroca

...oundary, Norian, Callovian, Aptian, Cretaceous-Cenozoic boundary, and Late Eocene. For each time interval both the general picture of the major plate tectoni ...l settings in the southern margin of the Tethys (below) at the time of the Eocene-Oligocene boundary (about 34 Ma).]]

* Generation-expulsion-migration: late Eocene-late Oligocene (40-25 Ma)

.... A compressive context predominates in the Eastern Cordillera since the [[Eocene]]. After the inversions of the Mesozoic extensional [[graben]]s, a thrust r

...stone reservoirs include Ventura and Los Angeles basins and Frigg field in Eocene of the North Sea.

...fluids.<ref name=Root_2007>Root, R. S., 2007, Geological evaluation of the Eocene Latrobe Group in the offshore Gippsland Basin for CO₂ geosequest

* Bradley, W. H., 1964, Geology of Green River Formation and associated Eocene rocks in southwestern Wyoming and adjacent parts of Colorado and Utah: U. S

...ef reservoirs are found in major oil fields such as the Oligocene to upper Eocene Kirkuk field of Iraq or the Lower Cretaceous fields found in the Golden Lan

...as targeted a shale resource system from the uppermost Paleocene–lowermost Eocene Waipawa Black Shale and Upper Cretaceous–lowermost Paleocene Whangai frac

.../BLTN15249/bltn15249.html Shale oil potential of lacustrine black shale in Eocene Dongying depression: Implications for geochemistry and reservoir characteri