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Information Journal Paper

Title

BIOSTRATIGRAPHY OF THE RUTEH FORMATION IN NORTH OF SHALAMZAR, CENTRAL ALBORZ BASED ON CONODONTS

Pages

  219-234

Abstract

 The RUTEH FORMATION in the North of SHALAMZAR is one of the fossiliferous Permian deposits in CENTRAL ALBORZ. Based on the lithological characteristics, this formation mainly consists of alternations of grey, medium to thick-bedded, fossiliferous limestones with cherts nodules, and can be subdivided into six rock units. This formation overlies unconformably the Dorud Formation and is covered disconformably by the Nesen Formation. According to international CONODONT biozone, two CONODONT biozones have been identified as follow:1) Sweetognathus whitei Zone (Artinskian=Yakhtashian).2) Ellisonia-Merilina Assemblage Zone (Early Artinskian-Late Murgabian).Sweetognathus whitei Zone can be coralated with international CONODONT biozonation (Wang Cheng et al., 1987).

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    APA: Copy

    HAMDI, BAHAEDDIN, VAZIRI, SEYED HAMID, & RANGRIZE AZARFAM, FARIDEH. (2012). BIOSTRATIGRAPHY OF THE RUTEH FORMATION IN NORTH OF SHALAMZAR, CENTRAL ALBORZ BASED ON CONODONTS. JOURNAL OF THE EARTH, 7(23), 219-234. SID. https://sid.ir/paper/193069/en

    Vancouver: Copy

    HAMDI BAHAEDDIN, VAZIRI SEYED HAMID, RANGRIZE AZARFAM FARIDEH. BIOSTRATIGRAPHY OF THE RUTEH FORMATION IN NORTH OF SHALAMZAR, CENTRAL ALBORZ BASED ON CONODONTS. JOURNAL OF THE EARTH[Internet]. 2012;7(23):219-234. Available from: https://sid.ir/paper/193069/en

    IEEE: Copy

    BAHAEDDIN HAMDI, SEYED HAMID VAZIRI, and FARIDEH RANGRIZE AZARFAM, “BIOSTRATIGRAPHY OF THE RUTEH FORMATION IN NORTH OF SHALAMZAR, CENTRAL ALBORZ BASED ON CONODONTS,” JOURNAL OF THE EARTH, vol. 7, no. 23, pp. 219–234, 2012, [Online]. Available: https://sid.ir/paper/193069/en

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