THE PETROLOGY OF ZIYARAN VOLCANIC BELT (ZVB) EOCENE VOLCANIC ROCKS

被引:0
作者
Shirjoposht, Leila Abbaspour [1 ]
Zakariaee, Sayed Jamal Al-Din Sheikh [2 ]
Ansari, Mohammad Reza [3 ]
Emami, Mohammad Hashem [2 ]
机构
[1] Islamic Azad Univ IAU, Geosci Dept, Sci & Res Branch, Tehran, Iran
[2] Islamic Azad Univ IAU, Fac Geosci Dept, Sci & Res Branch, Tehran, Iran
[3] Islamic Azad Univ IAU, Fac Geosci Dept, Chaloos Branch, Tehran, Iran
来源
REVISTA GEOARAGUAIA | 2021年 / 11卷 / 01期
关键词
ZIYARAN VOLCANIC BELT (ZVB); CENTRAL ALBORZ; PETROLOGY; EOCENE; OXIDATION-STATE; SILICATE LIQUIDS; OXYGEN FUGACITY; CLINOPYROXENES; IRAN; PETROGENESIS; EAST;
D O I
暂无
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
The Ziyaran Volcanic Belt (ZVB) is located in the southern part of central Alborz and in the Ziyaran area. The geology of this layer includes various kinds of stone units. In the north, they are the reminder of Cenozoic, quaternary deposits, and in the western part, the exposure stone units are mostly Precambrian and Paleozoic deposits and in the south-eastern part of the studied area, the stones belong to the Mesozoic era and specifically, the sediments belong to the Jurassic era are exposed. Also, the basic volcanic rocks that belong to the Eocene period are located in the Ziyaran area, in the western part of Taleqan County and in the Alborz state. This study aimed to evaluate the petrology of Ziyaran Volcanic Belt (ZVB) Eocene volcanic rocks. For this purpose, which is mostly focused on the study of Cretaceous stones in the central Alborz zone, sampling of the stones in the intended area was performed with the survey and field methods and for 120 samples. After the preparation of the thin layer from the well and without alteration samples, they were examined with petrography and petrology tests. The results of the petrology studies of the volcanic rocks of the Ziyaran area expressed that the basic volcanic rocks in the intermediate area with the intermediateupper chemical composition of Eocene Alkaline Phosphatase (ALP) located in the central zone of Alborz heights, with lithology composition of Alkali olivine basalts and Andesite.
引用
收藏
页码:77 / 94
页数:18
相关论文
共 37 条
[1]  
AGHA NABATI A., 2005, GEOLOGICAL MINERAL E, V1, P422
[2]  
AGHANABATI A., 2005, GEOLOGICAL MINERAL E, V1, P177
[3]  
ALAVI M, 1991, GEOL SOC AM BULL, V103, P983, DOI 10.1130/0016-7606(1991)103<0983:SASCOT>2.3.CO
[4]  
2
[5]  
AOKI K, 1973, PYROXENE LHERZOLITE
[6]   PETROLOGY AND PETROGENESIS OF SIAH KOOH VOLCANIC ROCKS IN THE EASTERN ALBORZ [J].
Baratian, Mostafa ;
Arian, Mohammad Ali ;
Yazdi, Abdollah .
GEOSABERES, 2020, 11 :349-363
[7]  
BERBERIAN M., 1981, GEODYNAMIC SERIES, Vs
[8]   The effect of water activity on the oxidation and structural state of Fe in a ferro-basaltic melt [J].
Botcharnikov, RE ;
Koepke, J ;
Holtz, F ;
McCammon, C ;
Wilke, M .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2005, 69 (21) :5071-5085
[9]  
Deer W.A., 1997, ROCK FORMING MINERAL, VSecond
[10]   POLYBARIC DIFFERENTIATION OF ALKALI BASALTIC MAGMAS - EVIDENCE FROM GREEN-CORE CLINOPYROXENES (EIFEL, FRG) [J].
DUDA, A ;
SCHMINCKE, HU .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1985, 91 (04) :340-353