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경남 거창분지 정장리 뢰스-고토양 연속층의 퇴적물 특성과 편년
황상일(Sangill Hwang),강창혁(Chang-Hyeok Kang),윤순옥(Soon-Ock Yoon) 대한지리학회 2011 대한지리학회지 Vol.46 No.1
대자율 및 압도분석, OSL 연대측정, 주원소, 희토류 및 미량원소 분석을 통해 거창 정장리 뢰스-고토양의 물리, 화학적 특징을 파악하였다. 거창 뢰스-고토양 연속층의 입도 특성은 하안단구를 형성하는 하천퇴적층 그리고 중국 뢰스고원과는 차이를 보인다. 뢰스-고토양 층서 가운데 L1과 L1L1은 MIS 2, L1S1은 MIS 3, L1L2는 MIS 4, S1은 MIS 5, L2는 MIS 6에 대비되므로 거창단면이 위치하는 하안단구는 MIS 7에 형성된 것으로 판단된다. 다만 MIS 3 시기에 남부지방이 중부지방보다 더 온난습윤하였을 가능성이 있다. 주원소와 희토류 원소, 미량원소 조성은 거창의 뢰스-고토양이 중국 뢰스고원보다 풍화가 더 많이 진행되었으며 중국 뢰스고원에서 기원하였음을 지시한다. 이것은 한반도의 다른 지역에서 이루어진 연구 결과와 조화된다. The physical and chemical characteristics of loess-paleosol sequence in Jeongjang-ri, Geochang basin are examined using the magnetic susceptibility measurement, grain size analysis, OSL age dating, major, rare earth and trace elements analysis. The grain size characteristics of the loess-palesol sequence are obviously different from those of river sediment forming river terrace deposits and the Chinese Loess Plateau. The loess-paleosol sequence consisting of L1, L1LL1, L1S1, L1L2, S1 and L2 from top to bottom is estimated to MIS 2~MIS 6 and the river terrace to MIS 7. The compositions of major, rare earth and trace elements indicate that the sequence show more weathered characteristics than the Chinese Loess Plateau and originated from the Chinese Loess Plateau. These features are in harmony with the previous studies in Korea.
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황상일 ( Sang Ill Hwang ),윤순옥 ( Soon Ock Yoon ),강창혁 ( Chang Hyeok Kang ),임원현 ( Won Hyeon Lim ) 한국지형학회 2010 한국지형학회지 Vol.17 No.4
대구광역시 북구 칠곡에 위치하는 팔계평야는 팔공산 가장자리를 둘러싼 환상산맥의 한 봉우리인 가산에서 발원하는 팔계천에 의해 형성된 범람원이다. 조사지역의 지형면은 자연제방과 배후습지 그리고 합류선상지로 구분되며, 자연제방과 선상지면은 청동기시대부터 인간생활의 주요한 공간으로 이용되었다. 팔계천 범람원 퇴적층은 하부에서부터 기반암, 하부역층, 하부사층, 하부실트층, 상부사력층, 표층인 상부실트층으로 세분된다. 하부역층은 최종빙기에 퇴적되었으며 나머지 층준은 홀로세 범람퇴적물이다. 선상지도 최종빙기에 형성되었다. 2000년대 이전의 토지경관은 지형면의 특징을 반영하였으나 이후에는 도시화로 인하여 거의 아파트단지가 조성되면서 지형경관은 크게 바뀌었다. The Palgye Plain, located in Chilgok, Buk-gu, Daegu-si, is a floodplain by Palgye-River rising from Mt. Ga one of the mountains in Ring Typed Mountains of Mt. Palgong. The geomorphic surfaces in the study area can be divided into the natural levee, back marsh and confluent fan, and the natural levee and fan have been used as important regions of human activities since the Bronze Age. The alluvium sediments of Palgye-River can be subdivided into the bedrocks, lower gravel deposits, lower sandy deposits, lower silty deposits, upper sand and gravel deposits, and upper silty deposits from the bottom according to the formative ages. The lower gravel deposits correlated to the last glacial stage and the rest to Holocene, respectively. Confluent fans were also formed during the last glacial stage. Moreover, The landscape with land use after 20C was changed to apartment area due to civilization differently from which reflected the characteristics of geomorphic surfaces in the past.
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姜昌赫 제주한라대학 1978 論文集 Vol.4 No.-
Those interested have made efforts to research for Tamla -Jeju- Spirit lately. I tried to find out the personality of Jeju islanders and the adjustment pattern of them in the mirror of Jeju-ballads. I divided their adjustment pattern into defense mechanism, rationalization mechanism, escape mechanism, aggression mechanism, and other adjustment mechanisms. According to those I divided them as 17 subcla ?? ifications again-daydreaming, identification, compensation, sublimation, projection, sour-grape, sweet-lemon, delusion, isolation, repression, regression, fixaation, obsession, direct-aggression, indirect-aggression, self-aggression, reaction-formation, etc. As the result of making analysis, study the ballads from the side of quantity, the main contents found out are as follows: 1) General tendency of Jeju islanders in the mirror of Jeju-ballads discovered in order of percentage was to the following effect: 30% at aggression mechanism, which was chiefly formed, 23% at escape mechanism, 22% at rationalization mechanism, 15% at defense mechanism, 6% at other reaction formation, etc., and it showed that Jeju islanders depended on aggressive adjustment pattern chiefly. 2) As the result of making analysis from 17 behaviour patterns, it showed following orders: 25% at indirect-aggression, 15% at sweet-lemon, 9% at isolation, 9% at compensation, 7% at repression, 6% at reaction formation, and other behaviour patterns. According to those, it is found out that the personality of Jeju islanders is chiefly formed with indirect-aggression and sweet-lemon, etc. 3) The personality of the islanders in the mirror of defense mechanism was showed in order of the following percent : 8% at Compensation behaviour, 4% at behaviour pattern of sublimation, identification .and daydreaming. It is very desired personality in the process of its formation that they try to cover frustration in their daily life with compensation behaiviour mainly. 4) The personality of Jeju islanders in the mirror of rationalization mechanism is as following orders; 15% at sweet-lemon, 4% at sour-grape. It proved that they have depended on the sweet-lemon-they ascribe their ill luck to fate if frustration happened to them. 5) The personality of Jeju islanders in the mirror of escape mechanism in showed as behaviour pattern of the following percentage: 9% at escape, 7% at repression, 3% at regression, and fixation, etc. It proved that they have solved their frustration in their daily life with escaping contact with others (isolation) or with patience (repression). 6) The personality of Jeju islander in the mirror of aggression mechanism is showed 25% at indirect-aggression, which is occupied chiefly, self-aggression, direct-aggression in order. It proved that ancestors of the islander did not criticize others for their conscience' sake directly, but make cynical remarks on them: by which they solved their daily problems-tension, anxiety, complication, etc. In conclusion the process of forming the personality of Jeju islander has chiefly depended on behabiour pattern of sweet lemon which ascribe their ill luck to fate, and the personality of them in the mirror of Jeju-ballads is indirect-aggression and reaction consciousness in a word.
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