Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

1,742
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

STRATIGRAPHY OF THE CRETACEOUS DEPOSITS IN HAFTAD GHOLLEH (EAST OF ARAK)

Pages

  94-107

Abstract

CRETACEOUS deposits are outcropped in HAFTAD GHOLLEH area, 25 km in the east of Arak city. In this study three stratigraphic sections were measured in the northeast, southeast and center of the area. Based on detailed study of stratigraphy and paleontology, in contrast to some other geologists’ opinion, it has been concluded  that  the CRETACEOUS deposits in this area can be divided into lower CRETACEOUS and upper units and distiguished well by their microfauna assemblages. The age of the Upper CRETACEOUS deposits is Early Cenomanian which conformably overlies the Early CRETACEOUS deposits. Also the Early CRETACEOUS succession is divided into basal part (detrial-carbonate) and upper part (carbonate with URGONIAN facies). The age of basal part, a barren zone, overlies dark shale and sandstone of Shemshak group with angular unconformity is Early CRETACEOUS (Neocomian?-Barremian) based on stratigraphic position and microfauna assemblage of the lowermost part of the CRETACEOUS carbonate sediments.The upper part of the Early CRETACEOUS succession based on identified fossil assemblages is devided into four BIOSTRATIGRAPHIC UNITs and consists of 9 BIOZONEs. The age of this part is Albian-Barremian.The beginning of transgrassive sea can be considered in Neocomian?-Barremian that lasted until Cenomanian. Tectonic occurrence of the MIDDLE CIMMERIAN leads to considrable angular unconformity in the basal part of the Lower CRETACEOUS deposits.

Cites

  • No record.
  • References

    Cite

    APA: Copy

    REZAEI ROUZBAHANI, P., & HAMDI, B.A.D.. (2008). STRATIGRAPHY OF THE CRETACEOUS DEPOSITS IN HAFTAD GHOLLEH (EAST OF ARAK). GEOSCIENCES, 17(68), 94-107. SID. https://sid.ir/paper/32390/en

    Vancouver: Copy

    REZAEI ROUZBAHANI P., HAMDI B.A.D.. STRATIGRAPHY OF THE CRETACEOUS DEPOSITS IN HAFTAD GHOLLEH (EAST OF ARAK). GEOSCIENCES[Internet]. 2008;17(68):94-107. Available from: https://sid.ir/paper/32390/en

    IEEE: Copy

    P. REZAEI ROUZBAHANI, and B.A.D. HAMDI, “STRATIGRAPHY OF THE CRETACEOUS DEPOSITS IN HAFTAD GHOLLEH (EAST OF ARAK),” GEOSCIENCES, vol. 17, no. 68, pp. 94–107, 2008, [Online]. Available: https://sid.ir/paper/32390/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top