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      • SEEING IS REMEMBERING? THE ROLE OF ATTENTION IN AUDIENCE MEMORY FOR PRODUCT PLACEMENT

        Sigen Song,Bin Xuan,Guoxin Ma,Wei Xu 글로벌지식마케팅경영학회 2018 Global Marketing Conference Vol.2018 No.07

        Similar to traditional advertising, product placement plays important roles in consumer purchasing behaviors through the AIDA model (e.g., Ghirvu,2013) of which attention is the very first stage. While there is an established literature on brand recall and recognition as methods of product placement evaluation, the role of attention, which is an important topic in traditional advertising research, has been sparsely studied in the context of product placement. This paper proposes that attention is a psychological state which affects information selection and processing. Captured attention reflects audience’s selective attention to editorial content including placements, while sustained attention (or processing) requires allocated attentional capacity to process information captured from the placement. When available attentional capacity is insufficient, product placements cannot be adequately processed to form accurate memory (Lee & Faber, 2007). Accordingly, this paper aims to investigate the pathway of ‘placement characteristics –audience attention – audience memory’ in order to reinterpret the relationship between placement characteristics and audience memory through the lens of attention. We do this by answering two pertinent questions: 1) how placement characteristics (e.g., exposure duration, frequency, location and size) influence captured attention; and, 2) how captured attention and sustained attention affect audience memory. To do so, we draw on psychology literature, especially the feature integration theory (Treisman & Gelade, 1980), in establishing the theoretical connections between placement features, captured attention, sustained attention and memory. By a theatre methodology, we found sustained attention mediated between captured attention and audience memory, while more prominent placement characteristics had stronger relationships with captured attention. Furthermore, audience’s levels of involvement in the media content and familiarity with the placed brand moderated the relationship between sustained attention and audience memory.

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        Mineralogical and geochemical study of hydrothermal dolomite from the Daliang zinc deposit in Guizhou, Southwest China: new evidence for the genesis

        Weijun He,Youguo Li,Sigen Ma 한국지질과학협의회 2023 Geosciences Journal Vol.27 No.2

        The Daliang zinc deposit occurs in the southwestern Xiangxi–Qiandong Zn-Pb metallogenic belt and is located on the southeastern margin of the upper Yangtze block. In this study, we present results from petrographic observations, rare earth elements, C-H-O isotopes, and fluid inclusions. The zinc deposit is hosted by middle Cambrian dolomite. The ore-forming process is divided into three stages from early to late: pyrite-galena, sphalerite-pyrite-dolomite, and dolomite. The characteristics of the REEs suggest that multiple fluids were involved in hydrothermal dolomite precipitation under low-temperature conditions. Two types of hydrothermal dolomite fluid inclusions were identified: pure liquid phase inclusions and liquid-rich phase inclusions. The fluid inclusions of hydrothermal dolomite yield homogenization temperatures of 108–192℃ (average 153℃), with salinities of 12.3–26.4 wt% (average 23.0 wt%) NaCl equiv. The δ13Cfluid, δDfluid and δ18Ofluid values for ore-forming fluids range from −4.2 to −3.5‰ (mean −3.8‰), −38.8 to −34.3‰ (mean −36.0‰), and 6.2–6.4‰ (mean 6.3‰), respectively. This study demonstrates that ore-forming fluid was sourced from a moderate- to high-salinity basinal brine and leached metals from metasedimentary rocks of the basement in the Yangtze block. The main transportation of ore-forming fluid occurred in the form of chlorine complexes along well-developed faults, and sulfides precipitated with decreases in pressure and temperature, as well as pH changes. Studies of the Daliang zinc deposit suggest that it is a mediumto low-temperature MVT-like deposit.

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