• 한국생활과학회지
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• 제22권4호
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• pp.609-618
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• 2013

The purpose of this study is to explore gender differences in elderly's dating experience and related variables. 427 elderly of age 65 or older participated. The results are as follows. 1. 80% of widowed elderly had no dating experience, and far more elderly men than women had dating experience. 2. Attitudes towards dating, of both elderly themselves and their children, had influence on the elderly's dating experience, regardless of gender. This indicates that the elderly's own acceptance and their children's positive attitude are important to the elderly's dating experience. 3. Gender differences were found in influences of living arrangement (whether they lived with their children or not), economical reasons, and personality factors. These variables proved significant only for the elderly men. More elderly men who did not live with their children than the elderly men who did had experienced dating, and economical reasons along with personality factors proved to be obstructive for elderly men's dating life.

• 가정과삶의질연구
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• 제34권4호
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• pp.51-75
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• 2016

This study focuses on the life experience of married women in their 30s to 40s who have experienced parental divorce. For a comprehensive understanding towards the women, this study takes a life history research approach. The participants of this research are 8 women who have experienced parental divorce and are now married with children. The data were gathered through in-depth interviews and were analyzed through the spiral of analysis, following the process of Wolcott's "description, analysis, and interpretation." The results of this study are as follows. First, participants experienced emotions such as fear, anger, and lack of affection. Second, parenting attitude and parental divorce had negative effects on the participants' formation and development of self concept and in turn, participants experienced anxiety and withdrawal from interpersonal relationships. Some had difficulties in concentrating on their schoolwork, which was caused by psychological effects from their instable home environments and some were negligent at school due to their parents' indifference or as an act of rebellion towards them. Third, although participants displayed interest towards the opposite sex, fear towards the opposite sex or unrealistic expectations led to difficulties in forming relationships. Participants also confessed that although they married so that they could escape their original family and form a new happy one, they experienced a rocky start at the beginning of their marriage. Fourth, parental divorce had a lifelong impact on children. Even after the children became adults, parental divorce affected each key stage of transition in life such as dating, choosing one's spouse, marriage, and child rearing. Fifth, participants displayed a strong attachment to life under the assumption that only they themselves can be depended on. This led to their strong commitments to a successful marriage without the possibility of divorce. In conclusion, parental divorce is not a transitory or incidental event. Rather, it becomes a part of the children's lives with lifelong implications.

• 자원환경지질
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• 제53권4호
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• pp.383-395
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• 2020

행매층은 실루리아기 회동리층과 오르도비스기 정선층(정선석회암) 사이에 위치하고 있어, 행매층의 층서적 위치는 회동리층의 존재와 시층서적 논란을 해결하는데 결정적 정보를 제공할 수 있다. 2011년 이후부터 행매층 존재와 함께 암층서 단위가 될 수 있는지에 대하여 논란이 있어왔다. 따라서 본 연구에서는 비룡동-평안리 사이 지역에 대한 정밀 지질조사를 통하여 행매층 분포와 지질구조 특성을 규명하고, 생층서와 절대연령 결과를 대비하여 행매층의 암층서 및 시층서적 의의를 정의하였다. 행매층을 대표하는 암석은 괴상의 황색-황갈색 함력 탄산염암으로 사암과 같은 입상조직을 가지고 있으며 노두 표면이 매우 거칠고 기공이 많이 발달하고 있다. 구성광물의 조성, 함량 및 미세조직 특징을 근거로 볼 때, 행매층의 특성은 역질의 쇄설암으로, 역은 돌로마이트이며 기질은 자형 및 반자형의 돌로마이트와 원마도 및 분급이 좋은 미사질의 석영이 주구성광물로 이루어져있다. 행매층은 조사지역인 정선군 정선읍 용탄리(비룡동)에서 평창군 미탄면 평안리까지 측방으로 연속하여 잘 발달하고 있을 뿐만 아니라 일정한 두께를 가지고 분포하고 있다. 행매층의 층리, 태위 및 층후는 비룡동-행매동 사이 지역에서는 회동리층과 거의 비슷하게 발달하나, 행매동 남서쪽에서는 등사습곡과 충상단층에 의하여 외견상 불규칙한 분포양상을 보인다. 즉 비룡동-행매동 사이에서는 340°±10°/15°의 태위를 유지하면서 200 m 층후로 발달하지만, 평안리 백암 일대에서는 동-서 1.5 km, 남-북 2.5 km에 달하는 넓은 면적을 차지하고 있다. 행매층 내 쇄설성 저어콘 U-Pb 연령은 470-450 Ma 범위를 갖고 있어 행매층의 최대 퇴적시기는 후기 오르도비스기를 지시한다. 또한, 행매층을 구성하는 함력 탄산염암은 쇄설성 퇴적암이므로, 행매층에서 분류된 중기 오르도비스기 코노돈트 화석군은 재퇴적된 이지성을 의미한다. 이는 행매층의 지질시대가 중기 오르도스기 이후 임을 지시한다. 본 연구 결과, 행매층은 전단대일 뿐이며, 정선석회암의 일부이고, 정선석회암과 동일한 시기를 갖는다는 부정적 학설은 타당성을 잃었으며, 행매층은 국제층서위원회(ICS)에서 제시한 층서기준에 적합하게 잘 정의된 암층서 단위임이 확인되었다.