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Fahliyan Formation

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Image
Published: 01 December 1965
Fig. 21. Type section of the Fahliyan Formation. N 30°11′19″ 51°27′36″
Image
Published: 01 December 1965
Fig. 24. —Type section of Fahliyan Formation. Kuh-e Dul, Fars Province. (Photo—A. J. Wells)
Image
Published: 02 April 2013
Fig. 10. ( a ) Final fault patterns identified from the neural network approach, displayed on the top Fahliyan Formation, together with a polar dip plot of interpreted faults. ( b ) A photo from extremely faulted and fractured Fahliyan Formation at the type section in Koohe Dal, located near
Journal Article
Published: 02 April 2013
Petroleum Geoscience (2013) 19 (2): 169–183.
...Fig. 10. ( a ) Final fault patterns identified from the neural network approach, displayed on the top Fahliyan Formation, together with a polar dip plot of interpreted faults. ( b ) A photo from extremely faulted and fractured Fahliyan Formation at the type section in Koohe Dal, located near...
FIGURES | View All (13)
Image
Published: 01 December 1965
Fig. 23. —Fine-grained limestone with Pseudocyclammina lituus (Yokoyama) (P), and small Trocholina sp. (T). Fahliyan Formation, Fars Province. Neocomian. ×50.
Image
Published: 10 October 2023
Figure 4. (a–d) Thin section and SEM images of the samples from the Ilam Formation with wackestone texture. (e–h) Packstone texture of the samples from the Sarvak Formation. (i–l) Packstone texture of the samples from the Fahliyan Formation. (m–t) The CT-scan image for interpreting the fracture
Image
Published: 10 October 2023
Figure 5. Results of the P- and S-wave velocity measurements on three samples taken from (a and d) the Ilam Formation, (b and e) the Fahliyan Formation, and (c and f) the Gadvan Formation, as obtained per mechanical tests. The blue curve shows the results of the constant differential pressure
Image
Published: 02 April 2013
Fig. 1. ( a ) Location of Dorood oil field in the northern part of the Persian Gulf. This field is 25 km long and 5 km wide and partly underlies Kharg Island. ( b ) Depth map of Fahliyan Formation, the main producing reservoir in the Dorood Field. Location of Figure 2 (X-Line 2000) is also
Image
Published: 02 April 2013
between the two wells. ( c ) A cross-section from the 3D permeability model from wells KG-43 through KG-47 shows that the most likely reason for the pressure difference is the sealing faults crossing the Fahliyan Formation.
Image
Published: 02 April 2013
) Ridge enhancement filter applied to top of Fahliyan Formation. This meta-attribute acts as an edge enhancer and is used to sharpen lineaments in a similarity cube. The ridge enhancement filter provides a more interpretable picture of faults and fractures.
Image
Published: 04 June 2015
1552.30 m, Dariyan Formation. ( d ) Favreina iranensis n. sp., paratype, WI–W7 field, depth 2471.21 m, Buwaib Formation. ( e ) Favreina sp., SR field, depth 2759.77 m, Fahliyan Formation. ( f ) Palaxius asmariensis n. sp., holotype, AB field, depth 864.05 m, Asmari Formation. ( g ) Palaxius sp. AB
Image
Published: 01 December 1965
Fig. 25. —Section exposing Fahliyan, Gadvan, Dariyan, Kazhdumi, and Sarvak Formations. Near Fahliyan village, Fars Province. (Photo—A. J. Wells)
Journal Article
Journal: Geophysics
Published: 10 October 2023
Geophysics (2023) 88 (6): MR323–MR332.
...Figure 4. (a–d) Thin section and SEM images of the samples from the Ilam Formation with wackestone texture. (e–h) Packstone texture of the samples from the Sarvak Formation. (i–l) Packstone texture of the samples from the Fahliyan Formation. (m–t) The CT-scan image for interpreting the fracture...
FIGURES | View All (13)
Journal Article
Published: 04 June 2015
Journal of Micropalaeontology (2015) 34 (2): 211–216.
... 1552.30 m, Dariyan Formation. ( d ) Favreina iranensis n. sp., paratype, WI–W7 field, depth 2471.21 m, Buwaib Formation. ( e ) Favreina sp., SR field, depth 2759.77 m, Fahliyan Formation. ( f ) Palaxius asmariensis n. sp., holotype, AB field, depth 864.05 m, Asmari Formation. ( g ) Palaxius sp. AB...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1965
AAPG Bulletin (1965) 49 (12): 2182–2245.
...Fig. 21. Type section of the Fahliyan Formation. N 30°11′19″ 51°27′36″ ...
FIGURES | View All (98)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2011
GeoArabia (2011) 16 (1): 151–203.
... Formation was proposed. Then, sequences of the Fahliyan Formation and their systems tracts were identified. Finally, compartments with more reservoir potential were recognized. The main tasks completed during this study are as follows: (1) study of microfossils (benthic foraminifera and algae); (2...
Image
Published: 01 December 1965
Fig. 27. Low-weathering limestone and shale of Gadvan Formation overlying massive Fahliyan limestone. Kuh-e Khami, north of Gachsaran.
Image
Published: 10 October 2023
Figure 8. Effect of geologic formation (i.e., Ilam, Sarvak, Laffan, Gadvan, and Fahliyan) on pore pressure coefficients of P- and S-wave velocities ( γ pu and γ su ): (a and d) static undrained bulk modulus, (b and e) static Young’s modulus, and (c and f) static Biot’s
Journal Article
Published: 01 August 2005
Petroleum Geoscience (2005) 11 (3): 225–238.
..., and the only one to be based on limited seismic data. A detailed review of all available data, including logs, revealed a number of features. The Dodrou and Rig wells were drilled on large and wide surface anticlines. They were drilled to the Fahliyan Formation of the Khami Group, where oil was found...
FIGURES | View All (25)
Journal Article
Journal: Clay Minerals
Published: 01 June 2005
Clay Minerals (2005) 40 (2): 191–203.
..., rhyolites, purple grey tuffaceous and micaceous sandstones and mudstones ( James & Wynd, 1965 ; Stocklin, 1968 ). The Khami Group comprising the Dariyan, Gadvan, Fahliyan and Surmeh Formations are the main Lower Cretaceous rock units of the southern Iran. The Fahliyan Formation (Neocomian...
FIGURES | View All (12)