Early Cretaceous Mineralizations in
Actinolite 39Ar-40Ar laser fusion technique was employed to determine the metallogenic epochs of the Ningwu porphyrite iron deposits. The 39Ar-40Ar isochron ages of the fresh actinolite (dark green) from the Dongshan iron deposit are from 126 to 129 Ma, which agree with the 39Ar-40Ar isochron age (127 Ma) of hornblende from the host volcanic rock of Dawangshan Group within the analytical errors, indicating that iron mineralization was associated with the Dawangshan Group volcanic rocks. The 39Ar-40Ar spectrum ages of altered actinolite (gray green) from the Washan iron deposit is (114±16) Ma. The two kinds of actinolites were formed at different metallization stages.