Fluid inclusion, mineralogical, geochemical, and isotopic (O, S) evidence for the genesis of the Khan-Khatun Zn-Pb deposit, Tabas Block, Iran
-
Published:2024-04
Issue:1
Volume:84
Page:126084
-
ISSN:0009-2819
-
Container-title:Geochemistry
-
language:en
-
Short-container-title:Geochemistry
Author:
Jamili Abdulmajid,
Aminzadeh BalandehORCID
Reference84 articles.
1. Transient, synobduction exhumation of Zagros blueschists inferred from P-T, deformation, time, and kinematic constraints: implications for Neotethyan wedge dynamics;Agard;J. Geophys. Res.,2006
2. Aghanabati, A., 2004. Geology of Iran. Geol. Surv. Iran (619 pp., in Persian with English abstract).
3. Evaluation of water source origin around Kerman tunnel, Iran: water transfer tunnel path using 2H, 3H, 18O, and 34S isotopes;Ahmadi;Arab. J. Geosci.,2021
4. Tectonics of the Zagros orogenic belt of Iran: new data and interpretations;Alavi;Tectonophysics,1994
5. The Triassic and associated rocks of the Nakhlak and Aghdarband areas in central and northeastern Iran as remnants of the southern Turonian active continental margin;Alavi;Geol. Soc. Am. Bull.,1997
Cited by
1 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献