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The Zhawulong granitic pegmatite lithium deposit is located in the Ganzi‐Songpan orogenic belt. Fluid inclusions in spodumene and coexisting quartz were studied to understand the cooling path and evolution of fluid within albite–spodumene pegmatite. There are three distinguishable types of fluid inclusions: crystal‐rich, CO2–NaCl–H2O, and NaCl–H2O. At more than 500°C and 350∼480 MPa, crystal‐rich...
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