| http://dbpedia.org/ontology/abstract
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지질기록은 행성의 지각에 있는 암석의 지층으로서 존재한다. 지질학은 지구의 … 지질기록은 행성의 지각에 있는 암석의 지층으로서 존재한다. 지질학은 지구의 역사와 형성을 밝히기 위해 암석의 나이와 기원에 관심을 기울인다. 지질시간은 행성의 지질학적 역사에서 날짜를 계산하기 위한 시간척도이며, 지구의 기원은 지금으로부터 약 46억 년 전으로 추산된다. 방사능 연대측정법은 물체의 방사성 원소의 지속적 붕괴를 측정하여 그 물체의 나이를 결정하는 방법으로, 지질기록에서 오래된 부분에 대해 날짜를 계산하는 데 사용된다. 이론적으로 매우 복잡하지만, 본질은 물체 안의 방사성 원소는 붕괴하여 각기 동위원소를 형성한다는 것이다. 동위원소는 일반적인 성질은 공유하지만 원자 질량이 다른 원소다. 지질학자들은 주로 탄소-14가 질소-14로 붕괴하는 것과 칼륨-40이 아르곤-40으로 붕괴하는 것을 사용한다. 탄소-14 측정법은 대략 5만 년 전 이후의 유기물질에 대해 사용된다. 더 오래된 기간에 대해서는 칼륨-아르곤 연대측정법이 사용된다. 방사능 연대측정은 기본적으로 물질에서 붕괴 이전과 붕괴 이후의 동위원소가 얼마나 많이 발견되는지 측졍하는 것이다. 양자의 비율을 통해 시료의 연대를 추정한다. 탄소연대측정을 위해 적합한 시료로는 목재, 목탄, 종이, 직물, 화석 등이 있다. 암석은 만들어진 순서에 따라 층층이 존재하며, 일반적으로 아래쪽일수록 오래된 층일 것으로 추정된다. 이것이 층서학의 기본이다. 보다 최근의 지층의 연대는 주로 암석 속에 보존된 고대 생명의 잔해인 화석을 연구하여 계산된다. 화석은 계속 발견되고 있기 때문에 이론이 유동적이다. 비교적 최근의 지질시대 경계는 기존 우점종(예컨대 공룡)의 절멸과 신종의 출현(예컨대 유인원)과 일치한다.기존 우점종(예컨대 공룡)의 절멸과 신종의 출현(예컨대 유인원)과 일치한다.
, This timeline of natural history summarizes significant geological and biological events from the formation of the Earth to the arrival of modern humans. Times are listed in millions of years, or megaanni (Ma).
, Esta é uma cronologia da história natural da Terra, que visa a relacionar os principais eventos geológicos e biológicos, significativos desde a formação da Terra até a chegada dos humanos modernos.
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| rdfs:comment |
This timeline of natural history summarizes significant geological and biological events from the formation of the Earth to the arrival of modern humans. Times are listed in millions of years, or megaanni (Ma).
, Esta é uma cronologia da história natural da Terra, que visa a relacionar os principais eventos geológicos e biológicos, significativos desde a formação da Terra até a chegada dos humanos modernos.
, 지질기록은 행성의 지각에 있는 암석의 지층으로서 존재한다. 지질학은 지구의 … 지질기록은 행성의 지각에 있는 암석의 지층으로서 존재한다. 지질학은 지구의 역사와 형성을 밝히기 위해 암석의 나이와 기원에 관심을 기울인다. 지질시간은 행성의 지질학적 역사에서 날짜를 계산하기 위한 시간척도이며, 지구의 기원은 지금으로부터 약 46억 년 전으로 추산된다. 방사능 연대측정법은 물체의 방사성 원소의 지속적 붕괴를 측정하여 그 물체의 나이를 결정하는 방법으로, 지질기록에서 오래된 부분에 대해 날짜를 계산하는 데 사용된다. 이론적으로 매우 복잡하지만, 본질은 물체 안의 방사성 원소는 붕괴하여 각기 동위원소를 형성한다는 것이다. 동위원소는 일반적인 성질은 공유하지만 원자 질량이 다른 원소다. 지질학자들은 주로 탄소-14가 질소-14로 붕괴하는 것과 칼륨-40이 아르곤-40으로 붕괴하는 것을 사용한다. 탄소-14 측정법은 대략 5만 년 전 이후의 유기물질에 대해 사용된다. 더 오래된 기간에 대해서는 칼륨-아르곤 연대측정법이 사용된다. 방사능 연대측정은 기본적으로 물질에서 붕괴 이전과 붕괴 이후의 동위원소가 얼마나 많이 발견되는지 측졍하는 것이다. 양자의 비율을 통해 시료의 연대를 추정한다. 탄소연대측정을 위해 적합한 시료로는 목재, 목탄, 종이, 직물, 화석 등이 있다.대측정을 위해 적합한 시료로는 목재, 목탄, 종이, 직물, 화석 등이 있다.
|
| rdfs:label |
Cronologia da história natural da Terra
, 자연사 연표
, Timeline of natural history
|
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http://dbpedia.org/resource/Geologic_time_scale +
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