7KHFHULXPULFKPLQHUDOEDVWQDVLWH

7KHFHULXPULFKPLQHUDOEDVWQDVLWHIRUPHGZLWKLQ ÀXRULWHFRSSHUVXO¿GHGHSRVLWVLQWKH*DOOLQDV0RXQWDLQV DERXWNPPLZHVWRIWKHWRZQRI&RURQDLQ/LQFROQ &RXQWFHQWUDO1HZ0H[LFR,Q±WKH*DOOLQDVPLQ-­ LQJGLVWULFWSURGXFHGVPDOODPRXQWVRIÀXRUVSDUULFKRUHIRU ÀXRULQHRXWSXWLVHVWLPDWHGWRKDYHEHHQOHVVWKDQWRQV PHWULFWRQV*ULVZROG'XULQJ±WKH &RQTXHURU1RFODLPSURGXFHGDSSUR[LPDWHOWRQV (54  metric  tons)  of  bastnasite  concentrate  from  these  same   ÀXRUVSDUGHSRVLWVZKLFKZDVSURFHVVHGQHDUELQ*DOOLQDV DWDVPDOOPLOORZQHGEWKH8QLWHG6WDWHV5DUH(DUWKV,QF *ULVZROG,QWKH1HZ0H[LFR&RSSHU&RUS produced  about  300  tons  (270  metric  tons)  of  copper-­lead-­ ÀXRUVSDURUHIURPLWV&RQTXHURUFODLPLQWKH*DOOLQDVGLVWULFW RIZKLFKDERXWWRQVPHWULFWRQVZDVEDVWQDVLWHRUH FRQFHQWUDWHIURPWKH&RQTXHURU1RFODLP 7KH*DOOLQDV0RXQWDLQVFRQVLVWRI/RZHU3HUPLDQVHGL-­ PHQWDUURFNVWKDWZHUHGRPHGXSOLIWHGIDXOWHGDQGIUDF-­ tured  during  the  emplacement  of  middle(?)  Tertiary  laccoliths   composed  mainly  of  alkaline  trachyte  and  rhyolite  (Perhac,   7KHÀXRULWHFRSSHUEDVWQDVLWHGHSRVLWVIRUPYHLQVDQG ¿OOEUHFFLDWHG]RQHVLQVDQGVWRQHVDQGVLOWVWRQHVRIWKH3HUP-­ LDQ

Kết quả (Việt) 1:

7KHFHULXPULFKPLQHUDOEDVWQDVLWHIRUPHGZLWKLQ ÀXRULWHFRSSHUVXO¿GHGHSRVLWVLQWKH*DOOLQDV0RXQWDLQV DERXWNP PL ZHVWRIWKHWRZQRI&RURQDLQ/LQFROQ &RXQWFHQWUDO1HZ0H[LFR,Q±WKH*DOOLQDVPLQ-­ LQJGLVWULFWSURGXFHGVPDOODPRXQWVRIÀXRUVSDUULFKRUH IRU ÀXRULQH RXWSXWLVHVWLPDWHGWRKDYHEHHQOHVVWKDQWRQV PHWULFWRQV  *ULVZROG 'XULQJ±WKH &RQTXHURU1RFODLPSURGXFHGDSSUR[LPDWHOWRQV (54 metric tons) of bastnasite concentrate from these same ÀXRUVSDUGHSRVLWVZKLFKZDVSURFHVVHGQHDUELQ*DOOLQDV DWDVPDOOPLOORZQHGEWKH8QLWHG6WDWHV5DUH(DUWKV,QF *ULVZROG ,QWKH1HZ0H[LFR&RSSHU&RUS produced about 300 tons (270 metric tons) of copper-­lead-­ ÀXRUVSDURUHIURPLWV&RQTXHURUFODLPLQWKH*DOOLQDVGLVWULFW RIZKLFKDERXWWRQV PHWULFWRQV ZDVEDVWQDVLWHRUH FRQFHQWUDWHIURPWKH&RQTXHURU1RFODLP 7KH*DOOLQDV0RXQWDLQVFRQVLVWRI/RZHU3HUPLDQVHGL-­ PHQWDUURFNVWKDWZHUHGRPHGXSOLIWHGIDXOWHGDQGIUDF-­ tured during the emplacement of middle(?) Tertiary laccoliths composed mainly of alkaline trachyte and rhyolite (Perhac,  7KHÀXRULWHFRSSHUEDVWQDVLWHGHSRVLWVIRUPYHLQVDQG ¿OOEUHFFLDWHG]RQHVLQVDQGVWRQHVDQGVLOWVWRQHVRIWKH3HUP-­ LDQ68 The Principal Rare Earth Elements Deposits of the United States *ODVVDQG6PDOOH6RXOH'H0DUN  Soule (1946) estimated that bastnasite forms about 5 percent of the breccia deposits. Soule (1946) analyzed hand-­picked grains of bastnasite from the Gallinas district and found that the bastnasite contained 74.39 percent total rare earth ele-­ PHQWVR[LGHVSHUFHQWFHULXPR[LGHDQGSHUFHQW other rare earth elements oxides. No resource estimate of the SRWHQWLDOÀXRUVSDUDQGEDVWQDVLWHWRQQDJHZLWKLQWKH*DOOLQDV district has been published

Kết quả (Việt) 2:

IRUPHG 7KH? FHULXP? ULFK? PLQHUDO? EDVWQDVLWH? ZLWKLQ? ÀXRULWH? FRSSHU VXO¿GH GHSRVLWV LQ WKH? * DOOLQDV? 0RXQWDLQV???? ?? NP DERXW ???? ????? PL RI ZHVW? WKH? WRZQ? RI? & RURQD? LQ? / LQFROQ? & RXQW ?? FHQWUDO? 1Hz? 0h [LFR ??, Q ????? ± ???? WKH? * DOOLQDV? PLQ- LQJ? GLVWULFW? SURGXFHG? VPDOO? DPRXQWV RI ÀXRUVSDU RUH??? ULFK? ? Iru? ÀXRULQH ?? RXWSXW? LV? HVWLPDWHG? WR? KDYH? EHHQ? OHVV? WKDQ ??????? WRQV? ??????? PHWULF? WRQV ?? * ULVZROG ?????? ?? 'XULQJ ????? ± ???? WKH? 1R ???? FODLP SURGXFHG DSSUR [LPDWHO ???? WRQV & RQTXHURU???? (54 tấn) của tập trung bastnasite từ những giống ÀXRUVSDU? ZDV GHSRVLWV ?? ZKLFK? SURFHVVHG QHDUE ? LQ? *? DOOLQDV? DW? D? VPDOO? PLOO E? RZQHG ? WKH? 8QLWHG? 6WDWHV? 5DUH? (DUWKV ??, QF ?? * ULVZROG ?????? ??, Q ??????? WKH? ? 0h [LFR? & RSSHU? & RUS ?? 1Hz? sản xuất khoảng 300 tấn (270 tấn) của LWV đồng-chì ÀXRUVSDU? RUH? IURP? & RQTXHURU? FODLP? LQ? WKH? * DOOLQDV? GLVWULFW ?? RI? DERXW ???? WRQV ????? PHWULF? WRQV? ZDV? EDVWQDVLWH? RUH? FRQFHQWUDWH? IURP? WKH? & 1R ????? FODLP? 7KH? * DOOLQDV? 0RXQWDLQV? FRQVLVW RI? RQTXHURU? ZKLFK? / RZHU? 3HUPLDQ? VHGL- PHQWDU ? URFNV? WKDW? ZHUH? GRPHG ?? XSOLIWHG ?? IDXOWHG ?? DQG? IUDF- tured trong emplacement của trung (?) laccoliths Tertiary gồm chủ yếu là trachyt kiềm và đá ryolit (Perhac, ???? ?? 7KH? ÀXRULWH? FRSSHU? EDVWQDVLWH? GHSRVLWV? IRUP? YHLQV? DQG? ¿OO? EUHFFLDWHG?] RQHV? LQ? VDQGVWRQHV? DQG RI? VLOWVWRQHV? WKH 3HUP- LDQ?68 Rare Tiền gửi Elements Trái đất chủ yếu của Hoa Kỳ
? * ODVV? DQG? 6PDOOH ???????? 6RXOH ???????? 'H0DUN ?????? ??? Soule (1946) ước tính rằng các hình thức bastnasite khoảng 5 phần trăm của các khoản tiền gửi -dăm kết. Soule (1946) đã phân tích hạt tay chọn của bastnasite từ huyện Gallinas và thấy rằng bastnasite chứa 74,39 phần trăm tổng số đất hiếm PHQWV tố? R [LGHV ???????? SHUFHQW R [DQG? FHULXP? LGH? ??????? SHUFHQW? khác yếu tố đất hiếm oxit. Không ước tính tài nguyên của SRWHQWLDO ÀXRUVSDU? DQG EDVWQDVLWH? WRQQDJH? ZLWKLQ? WKH? *? DOOLQDV? huyện đã được công bố