Return
Timing of magmatic–hydrothermal activity and gold mineralization at the Jiudian Gold Deposit, Jiaodong Peninsula, Eastern China: Constraints from integrated U–Pb and Rb–Sr geochronology
Z
Y
Z
Y
X
L
D
J
Z
DOI:10.1016/j.oregeorev.2026.107379.png)
Abstract
En 中文
• The newly identified skarn in the Jiudian gold deposit formed at ca. 145 Ma and is genetically linked to the Linglong granite. • Gold mineralization occurred at ca. 120 Ma, matching the emplacement age of adjacent mafic dikes and indicating a genetic relationship. • Two distinct magmatic-hydrothermal events are recognized in the deposit: barren skarn formation at ca. 145 Ma related to Linglong granites, and gold mineralization at ca. 119 Ma associated with mafic magmatism.
Keywords:
Jiaodong gold province
Jiudian gold deposit
Garnet U–Pb dating
In-situ mica Rb–Sr dating
Magmatic–hydrothermal evolution
AI Summary
Key information extracted from the uploaded paper, including a brief overview, abstract, background, key highlights, visual analysis, and future outlook.
Journal
IF:
3.6
Papers:
6.4K
Citations:
2.2W
