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Information Journal Paper

Title

FACIES ANALYSIS OF THE MIDDLE TO LATE CAMBRIAN TIDALITES IN ZARAND AREA - CENTRAL IRAN

Pages

  1-12

Abstract

 The Middle to Late CAMBRIAN deposits have several outcrops in Kerman Province - CENTRAL IRAN. These deposits have been introduced as KUHBANAN FORMATION. This formation has a thickness of about 330 meters in east of ZARAND city and has been studied for tidal facies analysis. The KUHBANAN FORMATION is disconformably overlain with Ordo-Silurian clastic deposits and also the formation is disconformably underlain by the Top Quartzites of the Early CAMBRIAN Dahu Formation. Based on stratigraphic studies, the KUHBANAN FORMATION is devided into 4 members in ZARAND area. All deposits in members 1 and 3 and some deposits of member 4 were formed in tidal flats. Field and petrographic studies of the Kuhbanan TIDALITES led to recognization of carbonate, siliciclastic, and mixed carbonate-siliciclastic facies groups.Detailed facies analysis of the KUHBANAN FORMATION resulted in recognition of three sequences (3rd order cycles) equivalent to the second half of the Sauk Sequence. After a global sea-level rising in the Late Early CAMBRIAN and during the expanding of shallow seas, these deposits were formed on the northern margin of the Gondwana Super Continent in a rift basin as homoclinal RAMP facies.

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    APA: Copy

    KOHANSAL GHADIMVAND, NADER. (2009). FACIES ANALYSIS OF THE MIDDLE TO LATE CAMBRIAN TIDALITES IN ZARAND AREA - CENTRAL IRAN. JOURNAL OF THE EARTH, 4(2), 1-12. SID. https://sid.ir/paper/192897/en

    Vancouver: Copy

    KOHANSAL GHADIMVAND NADER. FACIES ANALYSIS OF THE MIDDLE TO LATE CAMBRIAN TIDALITES IN ZARAND AREA - CENTRAL IRAN. JOURNAL OF THE EARTH[Internet]. 2009;4(2):1-12. Available from: https://sid.ir/paper/192897/en

    IEEE: Copy

    NADER KOHANSAL GHADIMVAND, “FACIES ANALYSIS OF THE MIDDLE TO LATE CAMBRIAN TIDALITES IN ZARAND AREA - CENTRAL IRAN,” JOURNAL OF THE EARTH, vol. 4, no. 2, pp. 1–12, 2009, [Online]. Available: https://sid.ir/paper/192897/en

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