RESTUDY OF MEMBERS 5 OF CHALUS FORMATION IN TYPE SECTION

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DARVISH ZADEH B.

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Journal: GEOSCIENCES Year:2001 | Volume:10 | Issue:41-42 Page(s): 60-65

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Information Journal Paper

Title

RESTUDY OF MEMBERS 5 OF CHALUS FORMATION IN TYPE SECTION

Author(s)

DARVISH ZADEH B. | Issue Writer Certificate

Keywords

STRATIGRAPHYQ2

PALEOGEOGRAPHYQ3

CHALUS FORMATIONQ4

IRANQ2

Abstract

In this article, STRATIGRAPHY and PALEOGEOGRAPHY of members 5 of CHALUS FORMATION has been studied. On the basis of stratigraphical position the member 5, is formed in the Middle- Upper Cenomanian time and consists of conglomerate and basic volcanic rocks with 500m. thickness.During the Cenomanian stage in the Chalus area (Northern flanks of Central Alborz) deep sea sedimentation was broken by several volcanic activities. These transformations caused to rise of the sea floor and created the temporary islands. After a little time, these lands went under water and Cenomanian deep sea covered all the islands again.

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APA: Copy

DARVISH ZADEH, B.. (2001). RESTUDY OF MEMBERS 5 OF CHALUS FORMATION IN TYPE SECTION. GEOSCIENCES, 10(41-42), 60-65. SID. https://sid.ir/paper/31453/en

Vancouver: Copy

DARVISH ZADEH B.. RESTUDY OF MEMBERS 5 OF CHALUS FORMATION IN TYPE SECTION. GEOSCIENCES[Internet]. 2001;10(41-42):60-65. Available from: https://sid.ir/paper/31453/en

IEEE: Copy

B. DARVISH ZADEH, “RESTUDY OF MEMBERS 5 OF CHALUS FORMATION IN TYPE SECTION,” GEOSCIENCES, vol. 10, no. 41-42, pp. 60–65, 2001, [Online]. Available: https://sid.ir/paper/31453/en

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