• 제목/요약/키워드: faulting

검색결과 131건 처리시간 0.023초

중국 연산지역의 인지운동(印支運動)의 특징 및 연산운동(燕山運動)과의 비교 (The Feature of Indosinian Movement and its comparison with Yanshanian Movement in the Yanshanian area, China)

  • 조성윤;김형식
    • 암석학회지
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    • 제6권1호
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    • pp.45-51
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    • 1997
  • 중생대 시기의 조구조 운동은 중국 동부 서태평양지역의 구조 발달사에 중요한 역할을 한 운동이다. 연산지역은 중생대의 전형적인 구조가 형성, 노출된 곳이며 쥬라기-백악기에 발생한 연산운동의 명명지이다. 과거에는 이 지역 대부분의 구조들은 연산운동에 의해 형성된 것으로 일반적으로 인정되어 왔지만, 다수의 습곡들은 삼첩기 후반에 발생한 인지운동에 의해 형성되었고 동시에 많은 대다수 단층들을 형성한 강렬한 활동이 있었음이 최근의 종합적 연구에 의해 밝혀졌다. 인지 운동이 발생한 조구조의 동역학적 환경은, 중·한지괴(Sino-Korean Massif)가 북쪽으로 이동하면서 대체로 E-W방향인 흥안-몽골 습곡대에 부딛쳐 생성된 N-S 방향의 압축응력 체제하에서 닫침 습곡(그 중 일부는 역전 습곡)이 형성되었으며, 연산운동의 몇차례 변형이 비공축(non-coaxial)으로 중첩(surperposed)되었다. 연산지역에서 중생대의 단층활동의 주요한 특성으로 인지운동시기에는 압축응력 작용에 의한 드러스트(thrust)가 주로 형성되었고, 연산운동시기에는 압축전단응력에 의한 사교 드러스트(oblique-thrust)가 주로 형성되었다.

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Microstructural Features and K-Ar Ages of Fault Gouges from Quaternary Faults along the Northern Yangsan Fault, SE Korea

  • Chang Oh Choo;Tae Woo Chang;Kounghoon Nam;Jong-Tae Kim;Chang-Ju Lee;Gyo-Cheol Jeong
    • 지질공학
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    • 제33권1호
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    • pp.121-136
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    • 2023
  • Microstructural characterization, identification of mineral assemblages, and K-Ar age dating of fault gouges from five Quaternary fault sites segmented along the northern Yangsan Fault, SE Korea were performed to understand formation condition and multiple activity of faults. The mean and median sizes of particles of bulk gouges vary among the studied faults: 1.75 ㎛ and 1.43 ㎛ for the Danguri Fault, 1.94 ㎛ and 1.79 ㎛ for the Yukjae Fault, 5.57 ㎛ and 4.16 ㎛ for the Yugye Fault, and 5.55 ㎛ and 2.31 ㎛ for the Bogyeongsa Fault. Fault gouges contain abundant secondary minerals, including smectite, chlorite, illite, kaolinite, laumontite, and mordenite, which are found in association with quartz and feldspar. K-Ar dating of the fault gouges (both bulk samples and separate size fractions) yields ages ranging from 59.1 to 18.8 Ma, with bulk ages of 47.6 Ma for the Yukjae Fault, 59.1 Ma for the Ansim Fault, 39.4 Ma for the Yugye Fault, and 22.6 Ma for the Bogyeongsa Fault. The finer fractions generally have younger K-Ar ages compared with the coarser fractions, and the finest fraction (<0.2 ㎛) is the youngest for each fault. Hydrothermal alteration of the gouges is considered to have occurred under low-temperature (100~200℃) conditions during faulting. Microstructural features and clay mineral assemblages of fault gouges and brecciated rocks should be considered when interpreting fault events and reactivation, in addition to age dating of faulting.

온도변화에 의한 콘크리트 포장도로의 구조 거동 연구 (Structural Behavior of Concrete Pavement Due to Temperature Variations)

  • 조병완
    • 전산구조공학
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    • 제4권2호
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    • pp.95-102
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    • 1991
  • 콘크리트 포장도로의 일부구간에서 보이고 있는 심각한 균열파괴현상은 주하중인 차량하중외에 환경요소인 온도변화의 영향으로, 콘크리트 슬래브 상, 하면의 온도차이에 따라 위, 아래방향으로 오목하게 휘면서, 기초지반과 떨어지는 슬래브의 중앙 또는 줄눈부에 차량하중이 재하되어 발생된다. 이로 인하여 콘크리트슬래브에 종적, 횡적 균열이 발생하여 Faulting, Ravelling, Spalling, Scaling..등 파괴 현상이 심화되고 있다. 따라서 본 연구에서는 유한요소법을 이용한 강성행렬과 온도변화, 건조수축등으로 인한 등가절점하중을 유도하여 전국 여러지방의 온도변화 특성에 따른 역학적 거동현상을 연구하였다.

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2001. 1. 26 인도지진 및 그 피해 특성 (Indian Earthquake(2001. 1. 26) and its damaged charateristics)

  • 전명순
    • 한국지진공학회:학술대회논문집
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    • 한국지진공학회 2001년도 춘계학술대회 논문집
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    • pp.3-9
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    • 2001
  • The Ms 7.7 earthquake of Gujarat, India occured early in the morning of January 26, 2001. Subsequent of the earthquake, as a Seismologist at Korea Institute of Geoscience and Mineral Resources(KIGAM), I have been visited epicentral area here reporting the impressions and initial observations collected during the period of Feb. 07 to 13. The trace of surface faulting was not founded. However the mechanism of the earthquake suggests the indenting Indian plate to the Eurasian plate was the tectonic background of this earthquake. Large casualties compare with the magnitude and focal depth of the event, seems due to the poor construction of the typical ordinary Indian housing structure. The wall and roof of the house are very thick to avoid high temperature of the epicentral region.

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양산단층 북부 유리계 일대의 신기 단층운동 소고 (Discussion on the Quaternary fault movement at Yugye-ri area in the northern part of Yangsan Fault)

  • 경재복
    • 한국지진공학회:학술대회논문집
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    • 한국지진공학회 2001년도 춘계학술대회 논문집
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    • pp.66-73
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    • 2001
  • Yangsan fault in the southeastern part of Korean peninsula has been locally reactivated along a prexisted fault during the late Pleistocene time. Geomorphological evidence of the reactivation is revealed at the northern segment(Yugye-ri, Tosung-ri areas) of the Yangsan fault. The reactivation is distinctively characterized by fault gouge and fracture zone with high frequency in the Yugye-ri area. Obique slip separation of the area is about three meters of the middle terrace. The cumulative vertical displacement is recognized after the formation of the middle terrace. Age of the reactivated faulting is constrained to during the formation of dissected valley deposits. Average vertical slip based on paleo-event is inferred to about 0.5-0.7 meter in this area.

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단층이란 무엇인가? (What is the Faults?)

  • 이병주;정장용
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2007년 가을학술발표회
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    • pp.127-137
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    • 2007
  • Faults are fractures along which there is visible offset by shear displacement parallel to the fracture surface. Faults can occur as single discrete breaks, but where the rock has been repeatedly faulted, or where the rock is especially weak, no discrete break may be evident. What forms instead is a fault zone composed of countless subparallel and interconnecting closely spaced fault surfaces. Faulting is fundamentally a brittle mechanism for achieving shear displacement. At deep crustal levels where rocks tend to deform plastically under conditions of elevated temperature and confining pressure, shear displacement is achieved by and development of shear zones. In this paper authors propose the fault grade in Korea.

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전기심사(電氣深査)에 의(依)한 함단층(含端層) 단층구조(斷層構造)의 전위측정(傳位測定)에 관(關)한 연구(硏究) (Potential Curves of Fault Coal Seam in Electrical Prospecting)

  • 서백수
    • 산업기술연구
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    • 제3권
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    • pp.9-15
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    • 1983
  • To detect faulted coal seam, two and three dimensional model experiments were conducted. The size of three dimensional water tank is $170cm{\times}80cm{\times}95cm$ and the size of model coal seam is $20cm{\times}50cm{\times}1cm$ carbon plate. In this paper, various potential curves were made changing distance and model size from surface. Using these curves, interpretation of faulting coal explotation in complex topography can be done by comparing field data each other.

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유한요소법에 의한 온도 하중의 해석 (A Finite Element Analysis Of Thermal Load On The Concrete Highway Pavement)

  • 조병완
    • 한국전산구조공학회:학술대회논문집
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    • 한국전산구조공학회 1991년도 봄 학술발표회 논문집
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    • pp.26-28
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    • 1991
  • In the recent years, a rigid pavement composed of a flat concrete slab has ken constructed due to the desirable structural strength of concrete, durability and economy. However, despite of precise design and construction of concrete highway pavement, some sections of the 88 Olympic express highway, Jung-bu express highway, and Kyung-bu express highway, which have shown premature cracking, faulting, and pumping before the end of their intended service life, have already been viewed with great concerns by highway officials and engineers. Since environmental variations and traffic loads might be considered as major factors to cause pavement failure problems, the thermal load due to temperature variations between top and bottom surface of the concrete slab was highlighted to verify analytical behavior of concrete slab using the finite element method.

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대륙 암권내의 융기지역에서 열응력 분포모델에 관한 연구 (An Analytical Model Study on the Thermal Stress around the Uplifted Province within the Continental Lithosphere)

  • 한욱
    • 자원환경지질
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    • 제24권1호
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    • pp.57-62
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    • 1991
  • 이 연구는 대륙 암권내에서 융기지역의 열응력 계산결과를 보여주며 주향방향의 연장선상에 2-D 가정하에 열탄성변위 포텐샬 함수를 이용하여 계산이 되었다. 연구로부터 얻은 열응력의 분포와 단층운동조건은 지열류량과 잘 일치하며, 대륙 암권내의 융기지역에서의 지열학적인 상태를 규명하는 데 중요한 역할을 한다.

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Simplified modelling of continous buried pipelines subject to earthquake fault rupture

  • Paolucci, Roberto;Griffini, Stefano;Mariani, Stefano
    • Earthquakes and Structures
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    • 제1권3호
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    • pp.253-267
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    • 2010
  • A novel simple approach is presented for the seismic analysis of continuous buried pipelines subject to fault ruptures. The method is based on the minimization of the total dissipated energy during faulting, taking into account the basic factors that affect the problem, namely: a) the pipe yielding under axial and bending load, through the formation of plastic hinges and axial slip; b) the longitudinal friction across the pipe-soil interface; c) the lateral resistance of soil. The advantages and drawbacks of the proposed method are highlighted through a comparison with previous approaches, as well as with finite element calculations accounting for the 3D kinematics of the pipe-soil-fault systems under large deformations. Parametric analyses are also provided to assess the relative influence of the various parameters affecting the problem.