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<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana">The conglomeratic sandstone sequences that overlie the regolith</SPAN></SPAN></STRONG></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana"> and host parts of U deposits are thoroughly oxidized terrestrial</SPAN></SPAN></STRONG></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana"> red bed sequences with very long and complex diagenetic and</SPAN></SPAN></STRONG></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana"> hydrothermal alteration histories.</SPAN></SPAN></STRONG></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana"> </SPAN></SPAN></STRONG></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana">----> The conglomeratic sandstone sequences have a very long</SPAN></SPAN></STRONG></SPAN></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana">history of complex diagenetic and hydrothermal alteration and have </SPAN></SPAN></STRONG></SPAN></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana">been thoroughly oxidized to become red bed sequences which are</SPAN></SPAN></STRONG></SPAN></SPAN><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana"> </SPAN></SPAN></STRONG></SPAN></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG><SPAN style="FONT-SIZE: 10pt"><SPAN style="FONT-FAMILY: Verdana">found on the regolith and many parts of U deposits on the land.</SPAN></SPAN></STRONG></SPAN></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG></STRONG></SPAN></SPAN> </P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><SPAN style="FONT-FAMILY: 함초롬바탕; FONT-SIZE: 10pt"><STRONG></STRONG></SPAN></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><STRONG><SPAN style="mso-fareast-font-family: 함초롬바탕"><SPAN style="FONT-SIZE: 10pt">표토와 </SPAN></SPAN><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; FONT-SIZE: 10pt; mso-font-width: 100%; mso-text-raise: 0pt">U </SPAN><SPAN style="FONT-SIZE: 10pt; mso-fareast-font-family: 함초롬바탕">퇴적지층의 많은 지역위에 분포하는 복합 사암 배열은 완전히 산화된</SPAN></STRONG></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><STRONG><SPAN style="FONT-SIZE: 10pt; mso-fareast-font-family: 함초롬바탕">육상 적색 암반 배열들로 매우 길고</SPAN><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; FONT-SIZE: 10pt; mso-font-width: 100%; mso-text-raise: 0pt">, </SPAN><SPAN style="FONT-SIZE: 10pt; mso-fareast-font-family: 함초롬바탕">복잡한 속성 작용에 의한 열수 변성 이력을 </SPAN></STRONG></P>
<P style="TEXT-AUTOSPACE: ; mso-pagination: none; mso-padding-alt: 0pt 0pt 0pt 0pt; tab-stops: left blank 371.6pt" class=0><STRONG><SPAN style="FONT-SIZE: 10pt; mso-fareast-font-family: 함초롬바탕">가지고 있다</SPAN></STRONG><SPAN style="LETTER-SPACING: 0pt; FONT-FAMILY: 함초롬바탕; mso-font-width: 100%; mso-text-raise: 0pt"><SPAN style="FONT-SIZE: 10pt"><STRONG>.</STRONG></SPAN></SPAN></P>
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13.01.08 23:11
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