BIOSTRATIGRAPHY OF LATE DEVONIAN SEQUENCE IN HUTK SECTION (NORTH OF KERMAN) BASED ON CONODONTS

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GHOLAMALIAN H.

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Journal: GEOSCIENCES Year:2006 | Volume:15 | Issue:59 Page(s): 94-101

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Title

BIOSTRATIGRAPHY OF LATE DEVONIAN SEQUENCE IN HUTK SECTION (NORTH OF KERMAN) BASED ON CONODONTS

Author(s)

GHOLAMALIAN H. | Issue Writer Certificate

Keywords

CONODONTSQ2

DEVONIANQ2

BIOSTRATIGRAPHYQ2

Abstract

Investigations on Hutk section prove the age of Middle Frasnian to Early Famennian for this section. Three genera and eighteen species have been obtained. Index species such as P. zinaidae and I. vitabilis show the age of Middle to Late Frasnian (hassi-linguiformis Zone) for the lower part of the section. Some of the Famennian index species such as P. semicostatus, I. camutus, I. iowaensis iowaensis and Pel. inclinatus reveal the age of Early Famennian (triangularis - Late crepida Zone).The new age ranges for some species have been determined in this paper. The earliest presence of I. iowaensis seems to be in Middle Frasnian and the range of P. alatus extends to Early Famennian. The oldest specimens of P. communis can be observed at the base of Hutk section by the age of Middle Frasnian.

Cites

LATE DEVONIAN CONODONTS FROM BAGHIN SECTION, WEST OF KERMAN

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APA: Copy

GHOLAMALIAN, H.. (2006). BIOSTRATIGRAPHY OF LATE DEVONIAN SEQUENCE IN HUTK SECTION (NORTH OF KERMAN) BASED ON CONODONTS. GEOSCIENCES, 15(59), 94-101. SID. https://sid.ir/paper/31396/en

Vancouver: Copy

GHOLAMALIAN H.. BIOSTRATIGRAPHY OF LATE DEVONIAN SEQUENCE IN HUTK SECTION (NORTH OF KERMAN) BASED ON CONODONTS. GEOSCIENCES[Internet]. 2006;15(59):94-101. Available from: https://sid.ir/paper/31396/en

IEEE: Copy

H. GHOLAMALIAN, “BIOSTRATIGRAPHY OF LATE DEVONIAN SEQUENCE IN HUTK SECTION (NORTH OF KERMAN) BASED ON CONODONTS,” GEOSCIENCES, vol. 15, no. 59, pp. 94–101, 2006, [Online]. Available: https://sid.ir/paper/31396/en

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