SEDIMENTARY SEQUENCES AND PALEOTEMPERATURE OF GADVAN FORMATION IN THE TYPE SECTION (GADAYUN MOUNTAIN, NE SHIRAZ)

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PARVANE NEZHADSHIRAZI M.; HEIDARI A.; MOSADEGH H.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Journal: JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK Year:2010 | Volume:2 | Issue:7 Page(s): 59-62

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Title

SEDIMENTARY SEQUENCES AND PALEOTEMPERATURE OF GADVAN FORMATION IN THE TYPE SECTION (GADAYUN MOUNTAIN, NE SHIRAZ)

Author(s)

PARVANE NEZHADSHIRAZI M. | HEIDARI A. | MOSADEGH H. | Issue Writer Certificate

Keywords

GADVAN FORMATIONQ3

SEQUENCE STRATIGRAPHYQ3

STABLE ISOTOPE VARIATIONQ3

SHIRAZQ3

GADAYUN MOUNTAINQ3

Abstract

The GADVAN FORMATION is a lithostratigraphic unit which is composed of limestone, shale, and marl. The boundary between Fahlyian and GADVAN FORMATIONs is gradual which is characterized by evidences of petrographic and isotopic analysis.No sharp fluctuation was witnessed in carbon and oxygen isotopic samples around the boundary and paleotemperature of GADVAN FORMATION using isotopic studies based on was estimated 27.5° C.Three depositional sequences have been identified in GADVAN FORMATION. These three sequences are bounded by type two boundary (SB2).

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APA: Copy

PARVANE NEZHADSHIRAZI, M., HEIDARI, A., & MOSADEGH, H.. (2010). SEDIMENTARY SEQUENCES AND PALEOTEMPERATURE OF GADVAN FORMATION IN THE TYPE SECTION (GADAYUN MOUNTAIN, NE SHIRAZ). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(7), 59-62. SID. https://sid.ir/paper/186825/en

Vancouver: Copy

PARVANE NEZHADSHIRAZI M., HEIDARI A., MOSADEGH H.. SEDIMENTARY SEQUENCES AND PALEOTEMPERATURE OF GADVAN FORMATION IN THE TYPE SECTION (GADAYUN MOUNTAIN, NE SHIRAZ). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2010;2(7):59-62. Available from: https://sid.ir/paper/186825/en

IEEE: Copy

M. PARVANE NEZHADSHIRAZI, A. HEIDARI, and H. MOSADEGH, “SEDIMENTARY SEQUENCES AND PALEOTEMPERATURE OF GADVAN FORMATION IN THE TYPE SECTION (GADAYUN MOUNTAIN, NE SHIRAZ),” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 7, pp. 59–62, 2010, [Online]. Available: https://sid.ir/paper/186825/en

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