Distinction of Magnetic Fabrics Produced by Primary Pyroclastic Processes and Contemporaneous Storm-Reworking Processes in a Coastal Tuff Ring,Jeju Island,Korea
Measurement of magnetic fabrics has been used to resolve the mechanisms of sediment transport and deposition and to distinguish between different depositional conditions (Rees, 1961, 1966; Rees et al., 1968; Hamilton and Rees, 1970). Magnetic shape factor (q-value), which is a measure of the strength of magnetic lineation,L(degree of long-axis alignment of magnetic grains), produced by tangential shear stress, relative to magnetic foliation, F (degree of short-axis alignment), produced by gravity force (Rees and Woodall, 1975), has been especially useful for sedimentological
magnetic fabric basaltic tuff storm reworking
Mi Eun Park Chanwoo Sohn Hyeongseong Cho Young Kwon Sohn
Department of Geology, Gyeongsang National University,Jinju, Korea Department of Geological Sciences, Pusan National University,Busan, Korea
国际会议
The 6th International Maar Conference(IMC)(第六届国际玛珥会议)
长春
英文
73-74
2016-07-30(万方平台首次上网日期,不代表论文的发表时间)