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해당 자료는 10페이지 까지만 미리보기를 제공합니다.
10페이지 이후부터 다운로드 후 확인할 수 있습니다.
10페이지 이후부터 다운로드 후 확인할 수 있습니다.
목차
Mineral Structures
Chemical Composition
Location in P – T Curve
Area of Talc & Serpentine
Chemical Composition
Location in P – T Curve
Area of Talc & Serpentine
본문내용
In P-T curve, Silicate minerals are a kind of Zeolite
Silicate minerals have many kind of group, But only this three mineral group have super ultra basic rock don't confuse with another situation. It's only ultra basic rack case.
In these three mineral groups, Olivin groub is go to green-schist area. Other thing is going to Blue-schist area. because basic rock have enough heavy metal mineral so when they deposition they want to high pressure
Olivin groub's have hydrophilic inter layer. so they can turn in low pressure. In a short, they have enough water
Silicate minerals have many kind of group, But only this three mineral group have super ultra basic rock don't confuse with another situation. It's only ultra basic rack case.
In these three mineral groups, Olivin groub is go to green-schist area. Other thing is going to Blue-schist area. because basic rock have enough heavy metal mineral so when they deposition they want to high pressure
Olivin groub's have hydrophilic inter layer. so they can turn in low pressure. In a short, they have enough water
키워드
- 가격5,000원
- 페이지수29페이지
- 등록일2010.06.18
- 저작시기2010.6
- 파일형식파워포인트(ppt)
- 자료번호#620305
본 자료는 최근 2주간 다운받은 회원이 없습니다.
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