LITHOFACIES ANALYSIS AND FINING UPWARD CYCLES OF SILICICLASTIC SEDIMENTS OF DAHU FORMATION (EARLY CAMBRIAN) EAST AND SOUTHEAST OF ZARAND, NWKERMAN

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MOUSAVI HARAMI SEYED REZA; MAHBOUBI ASAD ELAH; KHERADMAND ALI; ZAND MOGHADAM H.

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Journal: Iranian Journal of Geology Year:2008 | Volume:2 | Issue:6 Page(s): 71-85

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Title

LITHOFACIES ANALYSIS AND FINING UPWARD CYCLES OF SILICICLASTIC SEDIMENTS OF DAHU FORMATION (EARLY CAMBRIAN) EAST AND SOUTHEAST OF ZARAND, NWKERMAN

Author(s)

MOUSAVI HARAMI SEYED REZA | MAHBOUBI ASAD ELAH | KHERADMAND ALI | ZAND MOGHADAM H. | Issue Writer Certificate

Keywords

ARCHITECTURE ELEMENTSQ3

DAHU FORMATIONQ3

LITHOFACIESQ2

SILICICLASTICQ2

SEQUENCE SRATIGRAPHYQ2

Abstract

For LITHOFACIES analysis and recognization of ARCHITECTURE ELEMENTS of silisiclastic sediments of DAHU FORMATION (Late Camberian), two stratigraphy sections at Dahuieh (type section) and Gazuieh have been measured and the thickness are 240 and 227 meters, respectively. This study led to identification of 9 LITHOFACIES and 5 ARCHITECTURE ELEMENTS. LITHOFACIES classified into three categories including coarse grain (Gcm), medium grain (Sp, St, Sh, Sl, Sr, Sm), and fine grain (Fl, Fm). The interpreted ARCHITECTURE ELEMENTS are CH, LA, FF, CS, CR. Based on LITHOFACIES and ARCHITECTURE ELEMENTS, it is interpreted that these silisiclastic sediments may have been deposited in sand-bed meandering river. Sequence stratigraphy analysis show that the DAHU FORMATION formed during the sea level fall in the Early Camberian time. Many fining upward cycles, that have been formed the highstand system tract (HST), deposited during laterally migration of channel and subsidence of basin. We hope that this information can be used to basin analysis and paleogeographical reconstruction of the Early Camberian time in local and regional scales.

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

MOUSAVI HARAMI, SEYED REZA, MAHBOUBI, ASAD ELAH, KHERADMAND, ALI, & ZAND MOGHADAM, H.. (2008). LITHOFACIES ANALYSIS AND FINING UPWARD CYCLES OF SILICICLASTIC SEDIMENTS OF DAHU FORMATION (EARLY CAMBRIAN) EAST AND SOUTHEAST OF ZARAND, NWKERMAN. IRANIAN JOURNAL OF GEOLOGY, 2(6), 71-85. SID. https://sid.ir/paper/129418/en

Vancouver: Copy

MOUSAVI HARAMI SEYED REZA, MAHBOUBI ASAD ELAH, KHERADMAND ALI, ZAND MOGHADAM H.. LITHOFACIES ANALYSIS AND FINING UPWARD CYCLES OF SILICICLASTIC SEDIMENTS OF DAHU FORMATION (EARLY CAMBRIAN) EAST AND SOUTHEAST OF ZARAND, NWKERMAN. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2008;2(6):71-85. Available from: https://sid.ir/paper/129418/en

IEEE: Copy

SEYED REZA MOUSAVI HARAMI, ASAD ELAH MAHBOUBI, ALI KHERADMAND, and H. ZAND MOGHADAM, “LITHOFACIES ANALYSIS AND FINING UPWARD CYCLES OF SILICICLASTIC SEDIMENTS OF DAHU FORMATION (EARLY CAMBRIAN) EAST AND SOUTHEAST OF ZARAND, NWKERMAN,” IRANIAN JOURNAL OF GEOLOGY, vol. 2, no. 6, pp. 71–85, 2008, [Online]. Available: https://sid.ir/paper/129418/en

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