Premium
Zircon U–Pb Age and Deformation Characteristics of the J iama Porphyry Copper Deposit, T ibet: Implications for Relationships between Mineralization, Structure and Alteration
Author(s) -
Duan Jilin,
Tang Juxing,
Mason Russell,
Zheng Wenbao,
Ying Lijuan
Publication year - 2014
Publication title -
resource geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.597
H-Index - 43
eISSN - 1751-3928
pISSN - 1344-1698
DOI - 10.1111/rge.12043
Subject(s) - mineralization (soil science) , zircon , geology , geochemistry , copper , deformation (meteorology) , skarn , hornfels , mineralogy , hydrothermal circulation , fluid inclusions , metallurgy , seismology , materials science , biotite , paleontology , soil water , oceanography , soil science , quartz
The J iama copper deposit is one of the largest deposits recently found in T ibet and is composed of three types of mineralization including skarn, hornfels and porphyry. To investigate the relationship between mineralization, structure and alteration, we report new zircon U–Pb age and present field observations on the deformation characteritics associated with the copper mineralization in J iama. Two main periods of deformation were identified, represented by D 1 and D 2 in J iama. The first deformation ( D 1 ) occurred around 50 Ma, whereas the second deformation ( D 2 ) that was closely related to mineralization occurred later. Previous zircon U–Pb and molybnite Re–Os dating results indicate that the mineralizatoin occurred at ∼15 Ma and thus the D 1 regional deformation significantly occurred before the mineralization time, although the D 1 deformation probably provided important space for the development of significant copper deposition. Our new mapping and observations on the D 2 deformation demonstrate that the mineralization was closely coeval with or slightly later than the time of D 2 deformation. The new U–Pb zircon age further indicates that the aplite formed in ∼17.0 Ma and thus the D 2 deformation happened later than this time because the D 2 deformation cut across the aplite, which is proposed to be the key control for copper mineralization. Altered laminated hornfels including three types of alteration ( A ‐, K ‐ and S ‐type) were found spatially associated with the D 2 deformation. The type‐ A is mainly silicification, with fine sericite or chlorite, as well as abundant disseminated sulphides on fracture surfaces; the type‐ S is mainly fine‐grained silicification with patches of chlorite, epidote and common sulphides; the type‐ K (potassic alteration) appears to be fine‐grained biotite. Such types of alteration indicate the presence of skarns at depth where ore shoots are located. Taken together, the multiple structural‐magmatic‐mineralization events contributed to the formation of the supergiant J iama porphyry copper deposit in T ibet. The results have general implication for regional exploration.