文摘
To investigate the role of impurities on the deformation of calcite rocks, we performed creep experiments on fine-grained synthetic calcite aggregates with varying Mn-content. The tests were performed in a uniaxial creep apparatus at temperatures of 700aaa830 aaC and stresses between 15 and 65 MPa, resulting in strain rates of 10aaa7 to 10aaa4 saaa1. Varying the oxygen fugacity, fO2, between 10aaa18 and 10aaa4 MPa did not affect the creep strength. Applying a power law constitutive relationship on the creep data, two distinct creep regimes were observed, a low stress regime (<15 MPa) and a high stress regime (>20aaa25 MPa). In the low stress regime, a stress exponent n of 1.7aa0.3 and an activation energy of Q