STRUCTURAL FEATURES OF THE XIAOREQUANZI COPPER-DEPOSIT,XINJIANG

Jun. 1998

Article Contents

Article Navigation > Journal of Geomechanics > 1998 > 4(2): 83-90

Sun Liqian, Shang Ling, 1998. STRUCTURAL FEATURES OF THE XIAOREQUANZI COPPER-DEPOSIT,XINJIANG. Journal of Geomechanics, 4 (2): 83-90.

Citation:

Sun Liqian, Shang Ling, 1998. STRUCTURAL FEATURES OF THE XIAOREQUANZI COPPER-DEPOSIT,XINJIANG. Journal of Geomechanics, 4 (2): 83-90.

Citation:

Sun Liqian, Shang Ling, 1998. STRUCTURAL FEATURES OF THE XIAOREQUANZI COPPER-DEPOSIT,XINJIANG. Journal of Geomechanics, 4 (2): 83-90.

Abstract

The major structure in the mine district is NW-SE-trending disharmonic brachy anticlinorium superimposed by later N-S-trending second-order fold.NW trending minor faults as branch faults of E-W-trending major faults are well developed.The main ore deposit (No.1) is characterized by a duplex mineralization.The deposit is considered as a mesothermal filling-replacement copper deposit.
- duplex mineralization