CARBONATE FACIES OF THE SHALE UNIT OF THE LALUN FORMATION: NEW FINDINGS IN THYEH-DARVAR AREA (SOUTHWEST OF DAMGHAN)

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LASEMI Y.; AMIN RASOULI H.

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Journal: GEOSCIENCES Year:2005 | Volume:14 | Issue:54 Page(s): 70-79

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Title

CARBONATE FACIES OF THE SHALE UNIT OF THE LALUN FORMATION: NEW FINDINGS IN THYEH-DARVAR AREA (SOUTHWEST OF DAMGHAN)

Author(s)

LASEMI Y. | AMIN RASOULI H. | Issue Writer Certificate

Keywords

LALUN FORMATIONQ3

SHALE UNITQ4

TOP QUARTZITE UNITQ4

ESTUARYQ3

BIOHENNQ4

SEQUENCE STRATIGRAPHYQ4

Abstract

The SHALE UNIT of the LALUN FORMATION in Tuyeh-Darvar area (Southwest of Damghan) is unconformably underlain by the sandstone unit and is gradationally overlain by TOP QUARTZITE UNIT of the LALUN FORMATION. The SHALE UNIT of the LALUN FORMATION is composed of siliciclastic facies and two carbonate horizons (less than two meters thick) in the lower part of the SHALE UNIT. These carbonate horizons include dolomitized rnicrobialite and ooide grainstone facies, which were deposited in a ESTUARY environment of the northwestern passive margin of Gondwana, following late Early Cambrian mass extinction.

Cites

References

SEQUENCE STRATIGRAPHY OF THE SHALY AND TOP QUARTIZITE UNITS OF THE LALUN FORMATION IN TUYEH-DARVAR AREA (SOUTHWEST OF DAMGHAN)

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APA: Copy

LASEMI, Y., & AMIN RASOULI, H.. (2005). CARBONATE FACIES OF THE SHALE UNIT OF THE LALUN FORMATION: NEW FINDINGS IN THYEH-DARVAR AREA (SOUTHWEST OF DAMGHAN) . GEOSCIENCES, 14(54), 70-79. SID. https://sid.ir/paper/31678/en

Vancouver: Copy

LASEMI Y., AMIN RASOULI H.. CARBONATE FACIES OF THE SHALE UNIT OF THE LALUN FORMATION: NEW FINDINGS IN THYEH-DARVAR AREA (SOUTHWEST OF DAMGHAN) . GEOSCIENCES[Internet]. 2005;14(54):70-79. Available from: https://sid.ir/paper/31678/en

IEEE: Copy

Y. LASEMI, and H. AMIN RASOULI, “CARBONATE FACIES OF THE SHALE UNIT OF THE LALUN FORMATION: NEW FINDINGS IN THYEH-DARVAR AREA (SOUTHWEST OF DAMGHAN) ,” GEOSCIENCES, vol. 14, no. 54, pp. 70–79, 2005, [Online]. Available: https://sid.ir/paper/31678/en

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