MORPHOLOGY, CHEMISTRY AND GROWTH MECHANISMS OF CALCITE CONCRETIONS FROM AN INDUSTRIAL WATER-SOFTENING PROCESS: IMPLICATION FOR THE ORIGIN OF NATURAL OOIDS IS SEDIMENTS

RANKIN, A.H., & SUTCLIFFE, P.J.C.. (1999). MORPHOLOGY, CHEMISTRY AND GROWTH MECHANISMS OF CALCITE CONCRETIONS FROM AN INDUSTRIAL WATER-SOFTENING PROCESS: IMPLICATION FOR THE ORIGIN OF NATURAL OOIDS IS SEDIMENTS. PROCEEDING OF THE GEOLOGISTS ASSOCIATION, 110(1), 33-40. SID. https://sid.ir/paper/548810/en

RANKIN A.H., SUTCLIFFE P.J.C.. MORPHOLOGY, CHEMISTRY AND GROWTH MECHANISMS OF CALCITE CONCRETIONS FROM AN INDUSTRIAL WATER-SOFTENING PROCESS: IMPLICATION FOR THE ORIGIN OF NATURAL OOIDS IS SEDIMENTS. PROCEEDING OF THE GEOLOGISTS ASSOCIATION[Internet]. 1999;110(1):33-40. Available from: https://sid.ir/paper/548810/en

A.H. RANKIN, and P.J.C. SUTCLIFFE, “MORPHOLOGY, CHEMISTRY AND GROWTH MECHANISMS OF CALCITE CONCRETIONS FROM AN INDUSTRIAL WATER-SOFTENING PROCESS: IMPLICATION FOR THE ORIGIN OF NATURAL OOIDS IS SEDIMENTS,” PROCEEDING OF THE GEOLOGISTS ASSOCIATION, vol. 110, no. 1, pp. 33–40, 1999, [Online]. Available: https://sid.ir/paper/548810/en