{"id":3329,"date":"2025-05-14T16:25:40","date_gmt":"2025-05-14T08:25:40","guid":{"rendered":"https:\/\/quartz-grinding.epic-powder.com\/?post_type=astra-portfolio&p=3329"},"modified":"2025-05-15T15:21:31","modified_gmt":"2025-05-15T07:21:31","slug":"what-is-the-current-situation-of-jiangxi-which-has-rich-quartz-resources-how-should-it-be-developed-and-utilized","status":"publish","type":"astra-portfolio","link":"https:\/\/quartz-grinding.epic-powder.com\/tr\/astra-portfolio\/what-is-the-current-situation-of-jiangxi-which-has-rich-quartz-resources-how-should-it-be-developed-and-utilized\/","title":{"rendered":"Zengin kuvars kaynaklar\u0131na sahip olan Jiangxi'nin \u015fu anki durumu nedir? Nas\u0131l geli\u015ftirilmeli ve kullan\u0131lmal\u0131d\u0131r?"},"content":{"rendered":"

Kuvars genellikle d\u00fc\u015f\u00fck s\u0131cakl\u0131k kuvars\u0131n\u0131 (\u03b1 kuvars) ifade eder ve geni\u015f anlamda kuvars, y\u00fcksek s\u0131cakl\u0131k kuvars\u0131n\u0131 (\u03b2 kuvars) ve koeziti vb. de i\u00e7erir. Do\u011fada en yayg\u0131n kaya olu\u015fturan minerallerden biridir. Kuvars\u0131n ana bile\u015feni, renksiz ve \u015feffaf olan SiO2'dir, ancak baz\u0131 kapan\u0131mlar ve eser elementler nedeniyle genellikle farkl\u0131 renkler g\u00f6sterir. Genellikle beyaz, renksiz, dumanl\u0131, cams\u0131 ve k\u0131r\u0131k \u00fczerinde ya\u011fl\u0131d\u0131r. \u00d6zg\u00fcl a\u011f\u0131rl\u0131\u011f\u0131 2,22 ~ 2,65, Mohs sertli\u011fi 7,0, pH de\u011feri 6,0, erime noktas\u0131 1750\u2103'dir ve piezoelektrikli\u011fe sahiptir. Kuvars toksik de\u011fildir, kokusuzdur, kirlilik i\u00e7ermez, iyi s\u0131cakl\u0131k direncine, asit ve alkali korozyon direncine, zay\u0131f \u0131s\u0131 iletkenli\u011fine, y\u00fcksek yal\u0131t\u0131ma, d\u00fc\u015f\u00fck genle\u015fmeye, kararl\u0131 kimyasal \u00f6zelliklere ve y\u00fcksek sertli\u011fe sahiptir. Cam, refrakter malzemeler, seramik, d\u00f6k\u00fcm, kimya end\u00fcstrisi, \u00e7evre koruma, ta\u015flama, yap\u0131 malzemeleri ve di\u011fer end\u00fcstrilerde yayg\u0131n olarak kullan\u0131lmaktad\u0131r. Bunlar aras\u0131nda cam imalat end\u00fcstrisi ve yap\u0131 malzemeleri end\u00fcstrisi kuvars kaynaklar\u0131na b\u00fcy\u00fck bir talep g\u00f6stermektedir ve talep y\u0131ll\u0131k %8% oran\u0131nda artmaktad\u0131r. Y\u00fcksek kaliteli kuvars hammaddelerinden elde edilen y\u00fcksek safl\u0131ktaki kuvars, yar\u0131 iletkenler, havac\u0131l\u0131k, askeri, ileti\u015fim, fotovoltaik vb. gibi y\u00fcksek teknoloji end\u00fcstrilerinde yayg\u0131n olarak kullan\u0131lmaktad\u0131r ve stratejik olarak ortaya \u00e7\u0131kan bir malzeme olarak listelenmi\u015ftir. \u00dclkem \u015fu anda d\u00fc\u015f\u00fck kaliteli kuvars \u00fcr\u00fcnlerinde kendi kendine yetmektedir ve orta ila y\u00fcksek kaliteli \u00fcr\u00fcnler esas olarak ithalata dayanmaktad\u0131r (Hao Wenjun, 2020; Yan Lingya, 2020).<\/p>\n\n\n\n

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Jiangxi Eyaleti, uzun jeolojik ge\u00e7mi\u015fi, s\u0131k magmatik aktiviteleri ve belirgin metamorfizmas\u0131 olan Yangtze ve Huaxia plakalar\u0131 olmak \u00fczere iki antik levhay\u0131 kaplar ve \u00e7e\u015fitli genetik tiplerde kuvars kaynaklar\u0131 olu\u015fturur, \u00f6zellikle y\u00fcksek safl\u0131kta kuvars mineral hammaddelerinin olu\u015fumu i\u00e7in jeolojik ko\u015fullar olmak \u00fczere belirgin kaynak avantajlar\u0131na sahiptir. Bu makale, Jiangxi Eyaletindeki kuvars kaynaklar\u0131n\u0131n mevcut durumunu ve da\u011f\u0131t\u0131m \u00f6zelliklerini s\u0131ralar, kuvars kaynaklar\u0131n\u0131n mevcut uygulama durumunu analiz eder, granit kuvars ve kuvarsitin y\u00fcksek safl\u0131kta kuvars hammaddeleri olarak kullan\u0131lmas\u0131n\u0131n fizibilitesini tart\u0131\u015f\u0131r ve ayr\u0131ca eyalet d\u00fczeyinin ve sekt\u00f6rdeki meslekta\u015flar\u0131n dikkatini \u00e7ekmek amac\u0131yla Jiangxi Eyaletindeki kuvars kaynaklar\u0131n\u0131n geli\u015ftirilmesi ve kullan\u0131m\u0131 i\u00e7in \u00f6nerilerde bulunur.<\/p>\n\n\n\n

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Kaynak durumu ve da\u011f\u0131t\u0131m \u00f6zellikleri<\/h2>\n\n\n\n

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Jiangxi, kuvars kaynaklar\u0131 a\u00e7\u0131s\u0131ndan zengindir. End\u00fcstriyel tiplere g\u00f6re yedi kategori vard\u0131r: do\u011fal kristal, kuvarsit, kuvars kumta\u015f\u0131, kuvars kumu, toz kuvars, damar kuvars ve granit kuvars (Tablo 1). Jiangxi Eyalet Mineral Kaynaklar\u0131 Rezerv Tablosuna g\u00f6re (2019 sonu itibariyle), Jiangxi Eyaletinde 244 bilinen kuvars yata\u011f\u0131 bulunmaktad\u0131r (\u015eekil 1a), kan\u0131tlanm\u0131\u015f kaynak rezervleri ise 524.605,2 bin tondur (\u015eekil 1b). Mineral yataklar\u0131n\u0131n say\u0131s\u0131na bak\u0131ld\u0131\u011f\u0131nda, damar kuvars\u0131 yar\u0131dan fazlas\u0131n\u0131 olu\u015fturarak en b\u00fcy\u00fc\u011f\u00fcd\u00fcr, bunu s\u0131ras\u0131yla 22% ve 15% ile kuvarsit ve kuvars kumta\u015f\u0131, ard\u0131ndan 5%'den az ile toz kuvars ve kuvars kumu ve en az\u0131 ise yaln\u0131zca 1% ile do\u011fal kristal takip eder; Kan\u0131tlanm\u0131\u015f kaynak rezervleri a\u00e7\u0131s\u0131ndan kuvars kumta\u015f\u0131, kuvarsit ve kuvars kumu ba\u015fl\u0131calar\u0131d\u0131r ve \u00fc\u00e7\u00fcn\u00fcn toplam\u0131 toplam kan\u0131tlanm\u0131\u015f kaynaklar\u0131n 90%'sini olu\u015fturur. Di\u011ferleri s\u0131ras\u0131yla 6% ve 4%'sini olu\u015fturan damar kuvars ve toz kuvarst\u0131r. Do\u011fal kristalin kan\u0131tlanm\u0131\u015f kaynaklar\u0131 \u00e7ok k\u00fc\u00e7\u00fckt\u00fcr ve yakla\u015f\u0131k on binde birini olu\u015fturur. Jiangxi'nin kan\u0131tlanm\u0131\u015f kuvars kaynaklar\u0131 \u00fclkede \u00fcst s\u0131ralarda yer al\u0131r, bunlar\u0131n aras\u0131nda pembe kuvars ve damar kuvars 25%'den fazlas\u0131n\u0131 olu\u015fturarak \u00fclkede ilk s\u0131rada yer al\u0131r.<\/p>\n\n\n\n

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1.1 Do\u011fal kristal<\/h3>\n\n\n\n

Do\u011fal kristaller \u00e7o\u011funlukla kuvars damar tipi ve pegmatit tipidir. Kuvars damarlar\u0131nda geli\u015fen kristal ma\u011faralar\u0131 genellikle damar g\u00f6vdesinin geni\u015flemi\u015f k\u0131s\u0131mlar\u0131nda veya kesi\u015fimlerinde yer al\u0131r ve pegmatitlerde geli\u015fen kristal ma\u011faralar\u0131 genellikle \u00e7ekirdekte yer al\u0131r. Jiangxi'de \u00e7ok say\u0131da damar kuvars\u0131 ve pegmatit vard\u0131r ve bunlar yayg\u0131n olarak da\u011f\u0131lm\u0131\u015ft\u0131r. Kristal madenleri bir\u00e7ok kez ke\u015ffedilmi\u015ftir. 100'den fazla do\u011fal kristal mineral (kimyasal) noktas\u0131 ke\u015ffedilmi\u015ftir, ancak bunlar\u0131n \u00e7o\u011fu b\u00fcy\u00fck \u00f6l\u00e7ekli bir geli\u015fme olu\u015fturmad\u0131klar\u0131 i\u00e7in geli\u015ftirilmemi\u015f ve y\u00fcksek derecede kullan\u0131lmam\u0131\u015ft\u0131r. Bunlar\u0131n aras\u0131nda, yukar\u0131daki tabloda yer alan do\u011fal kristal madenleri yaln\u0131zca Lushan \u015eehri'ndeki Xiaomu Da\u011f\u0131 ve Gao'an \u015eehri'ndeki Dazu Mantou Da\u011f\u0131'd\u0131r. Madencilik alanlar\u0131ndaki kaynaklar t\u00fckenmi\u015f ve madencilik durdurulmu\u015ftur.<\/p>\n\n\n\n

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1.2 Kuvarsit<\/h3>\n\n\n\n

Kuvarsit, b\u00f6lgesel metamorfizma yoluyla kuvars kumta\u015f\u0131 veya di\u011fer silisli kaya\u00e7lar\u0131n yeniden kristalle\u015fmesiyle olu\u015fan, esas olarak kuvarstan olu\u015fan bir metamorfik kayad\u0131r. Jiangxi'de 157.263,56 bin ton kan\u0131tlanm\u0131\u015f kaynak rezervine sahip 53 kuvarsit yata\u011f\u0131 bulunmaktad\u0131r. Bilinen kuvarsit madenleri esas olarak Luoxiao-Zhuguang y\u00fckselmesinin Jinggangshan-Suichuan b\u00f6lgesinde ve Wuning, Xiushui, Lushan, Jing'an, Fengxin, Tonggu, Yifeng, Wanzai, Gao'an ve Jiuling y\u00fckselmesinin di\u011fer b\u00f6lgelerinde; Wugongshan y\u00fckselmesinin Pingxiang-Anfu b\u00f6lgesinde, Wuyi y\u00fckselmesinin Shicheng-Guangchang b\u00f6lgesinde, Wannian nap y\u00fckselmesinin Dexing-Leping b\u00f6lgesinde ve di\u011fer b\u00f6lgelerde da\u011f\u0131lm\u0131\u015ft\u0131r.<\/p>\n\n\n\n

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1.3 Kuvars kumta\u015f\u0131<\/h3>\n\n\n\n

Kuvars kumta\u015f\u0131, 90%'den fazla kuvars i\u00e7eri\u011fine sahip, konsolide deniz ve g\u00f6l tortul kumlu kayad\u0131r. Jiangxi'de 173.740,3 kilotonluk kan\u0131tlanm\u0131\u015f kaynak rezervine sahip 37 kuvars kumta\u015f\u0131 madeni bulunmaktad\u0131r. Bilinen kuvars kumta\u015f\u0131 madenleri \u00e7o\u011funlukla kuzeydo\u011fu Jiangxi'deki Leping, Yushan, Guangfeng, Guixi, Yiyang, Yujiang ve di\u011fer alanlarda ve Ji'an b\u00f6lgesinde da\u011f\u0131lm\u0131\u015ft\u0131r; kuzey Jiangxi'deki Ruichang, Tonggu ve g\u00fcney Jiangxi'deki Ruijin, Xinfeng, Quannan ve di\u011fer alanlarda da\u011f\u0131lm\u0131\u015flard\u0131r. Jiangxi'deki kuvars kumta\u015f\u0131 \u00e7o\u011funlukla ge\u00e7 Paleozoik'ten beri tortul \u00f6rt\u00fcde, \u00e7o\u011funlukla Devoniyen-Jura tabakalar\u0131nda bulunur. Cevher ta\u015f\u0131yan tabakalar aras\u0131nda Devoniyen Tiaomajian Formasyonu, Lingyan Temple Formasyonu, Yunshan Formasyonu, Zhongpeng Formasyonu, Zhangqiu Formasyonu, Yanghu Formasyonu, Guanshan Formasyonu, Leigutai Formasyonu, Karbonifer Outangdi Formasyonu, Permiyen Leping Formasyonu, Triyas Anyuan Formasyonu ve Jura Shuibei Formasyonu ve Zhangping Formasyonu yer almaktad\u0131r.<\/p>\n\n\n\n

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1.4 Kuvars kumu<\/h3>\n\n\n\n

Kuvars kumu, ana mineral bile\u015feni kuvars olan, granit, kuvarsit, kuvars kumta\u015f\u0131 ve damar kuvars\u0131n\u0131n do\u011fal a\u015f\u0131nmas\u0131 ve ta\u015f\u0131nmas\u0131yla olu\u015fan kum benzeri bir kuvars mineral hammaddesidir. Jiangxi'de 141.001,27 bin ton kan\u0131tlanm\u0131\u015f kaynak rezervine sahip 9 kuvars kumu madeni bulunmaktad\u0131r. Bilinen kuvars kumu madenleri \u00e7o\u011funlukla Hukou, Duchang, Lushan, Yongxiu vb. dahil olmak \u00fczere Poyang G\u00f6l\u00fc \u00e7evresindeki alana da\u011f\u0131lm\u0131\u015ft\u0131r. B\u00fcy\u00fck \u00f6l\u00e7ekli olanlar Yongxiu \u0130l\u00e7esindeki Songmen Adas\u0131 Kuvars Kumu Madencili\u011fi Alan\u0131 ve Hukou \u0130l\u00e7esindeki Zheji Kuvars Kumu Madencili\u011fi Alan\u0131'd\u0131r; di\u011ferleri Ruijin, Shanggao ve di\u011fer alanlara da\u011f\u0131lm\u0131\u015ft\u0131r. Jiangxi'deki kuvars kumu \u00e7o\u011funlukla modern g\u00f6llerdeki g\u00f6lsel tortul kuvars kumundan ve nehir boyunca al\u00fcvyonlu kumdan gelir. G\u00f6l olu\u015fumu ve nehir olu\u015fumu olarak ikiye ayr\u0131l\u0131r. G\u00f6l olu\u015fumu b\u00fcy\u00fck \u00f6l\u00e7ekli g\u00f6llerde en \u00e7ok geli\u015fmi\u015ftir. Poyang G\u00f6l\u00fc, zengin kuvars kumu kaynaklar\u0131na sahip \u00c7in'in en b\u00fcy\u00fck tatl\u0131 su g\u00f6l\u00fcd\u00fcr; Nehir olu\u015fumu, Ganjiang Nehri, Fuhe Nehri, Raohe Nehri, Xinjiang Nehri ve Xiuhe Nehri gibi be\u015f b\u00fcy\u00fck nehir gibi b\u00fcy\u00fck nehirlerde daha geli\u015fmi\u015ftir.<\/p>\n\n\n\n

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1.5 Pembe Kuvars<\/h3>\n\n\n\n

Pembe kuvars, son derece ince par\u00e7ac\u0131klar ve y\u00fcksek silisyum dioksit i\u00e7eri\u011fine sahip do\u011fal toz kuvarst\u0131r. Jiangxi'de 22.201,1 bin ton kan\u0131tlanm\u0131\u015f kaynak rezervine sahip 11 pembe kuvars madeni bulunmaktad\u0131r. Pembe kuvars madenlerinin \u00e7o\u011funlukla bat\u0131 Jiangxi'deki Pingxiang, Yichun, Lianhua, Anfu ve di\u011fer b\u00f6lgelerde; kuzeydo\u011fu Jiangxi'deki Wuyuan, Shangrao ve g\u00fcney Jiangxi'deki Xinfeng, Yudu ve di\u011fer b\u00f6lgelerde da\u011f\u0131lm\u0131\u015f oldu\u011fu bilinmektedir. Bunlar aras\u0131nda Pingxiang \u015eehri'ndeki Hejiatang, Yichun \u015eehri'ndeki Maitian, Anfu \u0130l\u00e7esi'ndeki Caijialing ve Xinfeng \u0130l\u00e7esi'ndeki Luofengtou'nun d\u00f6rt maden sahas\u0131 orta b\u00fcy\u00fckl\u00fcktedir. Jiangxi'deki pembe kuvars madeni, silisli kaya (mikrokristalin kuvarsit) yataklar\u0131n\u0131n ayr\u0131\u015fma tipine aittir (Fang Yesen, 2010) ve cevher ta\u015f\u0131yan tabakalar \u00e7o\u011funlukla Karbonifer-Permiyen tabakalar\u0131d\u0131r, \u00f6zellikle Orta Permiyen'deki Maokou Formasyonu ve Chetou Formasyonu'nun silisli kaya olu\u015fumunda yo\u011funla\u015fm\u0131\u015ft\u0131r.<\/p>\n\n\n\n

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1.6 Damar Kuvars<\/h3>\n\n\n\n

Damar kuvars\u0131 iri kristal par\u00e7ac\u0131klar\u0131na ve \u00e7ok saf kimyasal bile\u015fime sahiptir. SiO2 i\u00e7eri\u011fi genellikle 98%'nin \u00fczerindedir. Jiangxi'de 30.398,88 kilotonluk kan\u0131tlanm\u0131\u015f kaynak rezervine sahip 131 damar kuvars madeni bulunmaktad\u0131r. Damar kuvars madenlerinin \u00e7ok say\u0131da ve yayg\u0131n olarak da\u011f\u0131lm\u0131\u015f oldu\u011fu, \u00e7o\u011funlukla k\u00fc\u00e7\u00fck \u00f6l\u00e7ekli oldu\u011fu ve birka\u00e7 b\u00fcy\u00fck \u00f6l\u00e7ekli maden oldu\u011fu bilinmektedir. Sadece \u00fc\u00e7 orta b\u00fcy\u00fckl\u00fckte damar kuvars madeni vard\u0131r: Xingan \u0130l\u00e7esi'ndeki Dafengshan, Jinjiang Kasabas\u0131'ndaki Nankeng, Xiajiang \u0130l\u00e7esi ve Chongyi \u0130l\u00e7esi'ndeki Zhannao. Damar kuvars\u0131 genellikle magmatik hidrotermal etkiyle ili\u015fkilidir, \u00e7o\u011funlukla fay dolgusu boyunca olu\u015fmu\u015ftur ve en \u00e7ok granit ve metamorfik kaya alanlar\u0131nda geli\u015fmi\u015ftir. \u201cChina Mineral Geology: Jiangxi Volume\u201da g\u00f6re, Xiushui, Lushan, Wanzai, Gao'an, Xinyu, Chongren, Lichuan, Yushan ve di\u011fer yerlerdeki damar kuvars madenleri iyi kuvars kalitesine sahiptir ve cevher s\u00fct beyaz\u0131 ila renksiz, \u015feffaf ila yar\u0131 saydamd\u0131r ve SiO2 i\u00e7eri\u011fi 99%'den fazla ve Fe2O3 i\u00e7eri\u011fi 0.04%'den azd\u0131r. B\u00f6lgesel faylar ve y\u00fckseltilmi\u015f alanlardaki ikincil faylar genellikle b\u00fcy\u00fck \u00f6l\u00e7ekli damar kuvars madenleri olu\u015fturur. En b\u00fcy\u00fck arama umutlar\u0131 Mufu Da\u011f\u0131, Jiuling Da\u011f\u0131, Wugong Da\u011f\u0131, Wuyi Da\u011f\u0131, Yu Da\u011f\u0131 ve Nanling Da\u011f\u0131'ndad\u0131r.<\/p>\n\n\n\n

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1.7 Granit Kuvars<\/h3>\n\n\n\n

Granit, Jiangxi'de a\u015f\u0131r\u0131 geli\u015fmi\u015ftir ve 35.000 km2'lik a\u00e7\u0131k alan\u0131yla eyaletin alan\u0131n\u0131n 23.1%'sini olu\u015fturur. Di\u011fer kuvars t\u00fcrleriyle kar\u015f\u0131la\u015ft\u0131r\u0131ld\u0131\u011f\u0131nda, granit kuvars \u00f6nemli \u00f6l\u00e7ek avantajlar\u0131na ve geli\u015ftirme ve kullan\u0131m i\u00e7in geni\u015f beklentilere sahiptir. Ancak, d\u00fc\u015f\u00fck i\u00e7eri\u011fi (genellikle 20-35%) nedeniyle, granit kuvars\u0131n mevcut geli\u015ftirme ve kullan\u0131m seviyesi nispeten d\u00fc\u015f\u00fckt\u00fcr ve esas olarak at\u0131k ve ili\u015fkili mineraller olarak kullan\u0131l\u0131r.<\/p>\n\n\n\n

\"\"<\/figure>\n\n\n\n

Kuvars uygulamas\u0131n\u0131n g\u00fcncel durumu ve y\u00fcksek safl\u0131kta kuvars hammaddelerinin se\u00e7imi<\/h2>\n\n\n\n

End\u00fcstriyel tipteki kuvars yataklar\u0131, end\u00fcstriyel uygulamalar\u0131n \u00f6zellikleriyle yak\u0131ndan ili\u015fkilidir. Wang Ling, end\u00fcstriyel uygulamalar\u0131n \u00f6zelliklerini, farkl\u0131 end\u00fcstriyel tipteki yataklar\u0131n kuvars \u00f6zelliklerine dayanarak \u00f6zetlemi\u015ftir (Wang Ling, 2019). Y\u00fcksek safl\u0131kta kuvars, ulusal stratejik end\u00fcstrilerin ve temel end\u00fcstrilerin geli\u015fiminde yeri doldurulamaz bir temel malzemedir. Yar\u0131 iletken yongalar, g\u00fcne\u015f fotovoltaikleri, optik fiber ileti\u015fim, havac\u0131l\u0131k, hassas optik ve \u00f6zel cam gibi y\u00fcksek teknoloji end\u00fcstrileri i\u00e7in vazge\u00e7ilmez ve yeri doldurulamaz \u00f6nemli bir i\u015flevsel malzemedir. Ger\u00e7ekten "boyun s\u0131k\u0131\u015fm\u0131\u015f" bir mineral kayna\u011f\u0131d\u0131r. \u00d6nemli stratejik konumu nedeniyle, silisyum dioksitte "dev panda" olarak adland\u0131r\u0131l\u0131r (Wang Jiuyi, 2022). Y\u00fcksek safl\u0131kta kuvars hammaddeleri, safla\u015ft\u0131rma s\u00fcre\u00e7leri yoluyla y\u00fcksek safl\u0131kta kuvarstan \u00e7\u0131kar\u0131labilen kuvars hammaddelerini ifade eder. Y\u00fcksek safl\u0131kta kuvars hammaddeleri \u00fczerine yap\u0131lan ara\u015ft\u0131rmalar, \u015fu anda \u00fclkemdeki kuvars ara\u015ft\u0131rmalar\u0131n\u0131n s\u0131n\u0131r y\u00f6n\u00fcd\u00fcr (Chen Junyuan, 2020; Wang Jiuyi, 2021). Do\u011fal kristal, y\u00fcksek safl\u0131kta kuvars \u00fcretmek i\u00e7in orijinal hammaddeydi, ancak k\u00fc\u00e7\u00fck rezervleri ve y\u00fcksek fiyatlar\u0131 nedeniyle, b\u00fcy\u00fck \u00f6l\u00e7ekli end\u00fcstriyel \u00fcretimin ihtiya\u00e7lar\u0131n\u0131 kar\u015f\u0131lamak zordu. Wang Ling (2014), damar kuvars ve granit kuvars\u0131n, y\u00fcksek safl\u0131kta kuvars orta ve \u00fcst d\u00fczey \u00fcr\u00fcnlerini i\u015flemek i\u00e7in do\u011fal kristalin yerini alacak ideal hammaddeler oldu\u011funu, ancak t\u00fcm damar kuvars ve granit kuvars\u0131n y\u00fcksek safl\u0131kta kuvars\u0131 i\u015fleyemeyece\u011fini belirtti. \u00c7ok az say\u0131da veya \u00e7ok az say\u0131da ara\u015ft\u0131rmac\u0131 y\u00fcksek kaliteli \u00fcr\u00fcnleri i\u015fleyebilir. \u00d6nceki ara\u015ft\u0131rmac\u0131lar (Tian Qingyue, 2017; Wang Ting, 2018; Wang Yunyue, 2020) y\u00fcksek safl\u0131kta kuvars hammaddesi olarak damar kuvars\u0131 \u00fczerinde \u00e7ok say\u0131da ara\u015ft\u0131rma y\u00fcr\u00fctm\u00fc\u015f ve dikkate de\u011fer sonu\u00e7lar elde etmi\u015f, ancak granit kuvars ve kuvarsit \u00fczerindeki ara\u015ft\u0131rmalar nispeten azd\u0131r. Son y\u0131llarda, Jiangxi Jeolojik Ara\u015ft\u0131rma Enstit\u00fcs\u00fc ilgili ara\u015ft\u0131rma \u00e7al\u0131\u015fmalar\u0131n\u0131 y\u00fcr\u00fctm\u00fc\u015f ve belirli jeolojik ko\u015fullar alt\u0131nda olu\u015fan granit kuvars ve kuvarsitin potansiyel olarak elveri\u015fli y\u00fcksek safl\u0131kta kuvars hammaddeleri oldu\u011funa inanmaktad\u0131r.<\/p>\n\n\n\n

<\/p>\n\n\n\n

2.1 Granit Kuvars<\/h3>\n\n\n\n

Granit kuvars, yava\u015f kristalle\u015fmesi ve uzun s\u00fcresi nedeniyle y\u00fcksek safl\u0131kta kuvars \u00e7\u0131karmak i\u00e7in ideal bir hammaddedir ve nispeten saft\u0131r. D\u00fcnyan\u0131n en \u00fcnl\u00fc IOTA serisi y\u00fcksek safl\u0131kta kuvars kumu, Amerika Birle\u015fik Devletleri'nin Spruce Pine b\u00f6lgesindeki beyaz granitten gelir. Yurt i\u00e7i ara\u015ft\u0131rma sonu\u00e7lar\u0131, belirli jeolojik ko\u015fullar alt\u0131nda olu\u015fan granit kuvars\u0131n y\u00fcksek safl\u0131kta kuvars \u00e7\u0131karmak i\u00e7in kullan\u0131labilece\u011fini do\u011frulam\u0131\u015ft\u0131r (Zhang Ye, 2012; Zhang Yanyan, 2018; Cong Jinyao, 2019; Zhao Jinzhou, 2022). Yazar, kapsaml\u0131 ara\u015ft\u0131rma ve incelemeden sonra, pegmatit, pegmatit granit ve muskovit pegmatit granitin potansiyel olarak elveri\u015fli y\u00fcksek safl\u0131kta kuvars hammaddeleri oldu\u011funa inanmaktad\u0131r. Yihuang Tangyin ve Ningdu Wangxi K\u00f6y\u00fc taraf\u0131ndan temsil edilen b\u00fcy\u00fck \u00f6l\u00e7ekli ve y\u00fcksek kaliteli y\u00fcksek safl\u0131kta kuvars hammaddeleri ke\u015ffedilmi\u015ftir. Yihuang Tangyin pegmatiti\u2460 ku\u015faklar halinde da\u011f\u0131lm\u0131\u015f olup orta-ince taneli biyotit monzogranitin i\u00e7ine girmektedir. B\u00fcy\u00fck damar benzeri ve kistik olan, uzun ekseni NEE e\u011filimli, 265-650 metre uzunlu\u011funda, 6-80 metre geni\u015fli\u011finde ve genel olarak NNW e\u011fimli ve yerel olarak SSE e\u011fimli 5 b\u00fcy\u00fck \u00f6l\u00e7ekli pegmatit vard\u0131r. Olu\u015fum nispeten diktir, genellikle 65-85\u00b0. Pegmatitler esas olarak feldispat, kuvars ve muskovitten olu\u015fur, ard\u0131ndan karakteristik mineral olarak granat ile turmalin gelir. Tangyin pegmatitindeki y\u00fcksek kaliteli kuvars\u0131n ana safs\u0131zl\u0131k elementleri, 99.992% veya daha fazla y\u00fcksek safl\u0131kta kuvarsa safla\u015ft\u0131r\u0131lma potansiyeline sahip olan Al54.34\u00d710-6, Li0.34\u00d710-6 ve Ti25.46\u00d710-6'd\u0131r; genel kuvars\u0131n safs\u0131zl\u0131k elementleri, 99.98% veya daha fazla y\u00fcksek safl\u0131kta kuvarsa safla\u015ft\u0131r\u0131lma potansiyeline sahip olan Al54-200\u00d710-6, Li0.33-17\u00d710-6 ve Ti3-40\u00d710-6'd\u0131r. Ningdu\u2461, Wangxi K\u00f6y\u00fc'ndeki beyaz mika pegmatit graniti, d\u00fczensiz eliptik bir d\u00fczleme, yak\u0131n do\u011fu-bat\u0131 e\u011filimine, 300 metreden fazla uzunlu\u011fa ve yakla\u015f\u0131k 160 metre geni\u015fli\u011fe sahip bir kaya t\u00fcm\u00f6r\u00fc \u015feklinde \u00fcretilmi\u015ftir. Orta iri taneli porfirik biyotit monzonit granitinde bulunur. Beyaz mika pegmatitinin ana mineralleri feldispat, kuvars ve beyaz mikad\u0131r ve \u00e7ok az koyu mineral vard\u0131r. Wangxi K\u00f6y\u00fc muskovit pegmatit granit kuvars\u0131n\u0131n ana safs\u0131zl\u0131k elementleri Al54.94\u00d710-6, Ti13.71\u00d710-6 ve Li1.03\u00d710-6'd\u0131r ve 99.991%'nin \u00fczerinde y\u00fcksek safl\u0131kta kuvarsa safla\u015ft\u0131r\u0131lma potansiyeline sahiptir ve b\u00fcy\u00fck \u00f6l\u00e7ekli veya \u00fczerinde olmas\u0131 \u00f6ng\u00f6r\u00fclmektedir.<\/p>\n\n\n\n

<\/p>\n\n\n\n

2.2 Kuvarsit<\/h3>\n\n\n\n

Kuvarsit, kuvars kumta\u015f\u0131 veya di\u011fer silisli kaya\u00e7lar\u0131n metamorfizmas\u0131yla olu\u015fur. Metamorfizma, kuvarstaki orijinal safs\u0131zl\u0131k elementlerinin g\u00f6\u00e7 etmesine neden olarak kuvars\u0131n safl\u0131\u011f\u0131n\u0131 art\u0131r\u0131r. M\u00fclleretal (2007), Norve\u00e7'in kuzeyindeki kyanit kuvarsitini inceledi ve kuvarstaki safs\u0131zl\u0131k element i\u00e7eri\u011finin d\u00fc\u015f\u00fck oldu\u011funu, birka\u00e7 s\u0131v\u0131 kapan\u0131m bulundu\u011funu ve kuvars ile di\u011fer mineraller aras\u0131ndaki tane s\u0131n\u0131rlar\u0131n\u0131n \u00e7o\u011funlukla d\u00fcz oldu\u011funu buldu. Yang Xiaoyong (2021), retrograd metamorfizman\u0131n kuvars\u0131n orijinal eser element bile\u015fimini etkiledi\u011fine inanmaktad\u0131r. Retrograd metamorfizma s\u0131ras\u0131nda kuvars, tane s\u0131n\u0131r\u0131 alan\u0131n\u0131n k\u00fc\u00e7\u00fclmesi ve tane s\u0131n\u0131rlar\u0131n\u0131n g\u00f6\u00e7\u00fcyle birlikte kafes iyile\u015fmesine u\u011frar, bu da kuvars\u0131n kafes kusurlar\u0131n\u0131 iyile\u015ftirmeye ve kafesteki safs\u0131zl\u0131k elementlerini (Al, Ti vb. gibi) tane s\u0131n\u0131r\u0131na atmaya veya bunlar\u0131 kapan\u0131mlara yo\u011funla\u015ft\u0131rmaya elveri\u015flidir. Jiangxi'deki kuvarsit, esas olarak Prekambriyen metamorfik tabakalar\u0131nda da\u011f\u0131lm\u0131\u015ft\u0131r. Temsili kuvarsit ta\u015f\u0131yan tabakalar aras\u0131nda, merkezi ve g\u00fcney Jiangxi'de yayg\u0131n olarak da\u011f\u0131lm\u0131\u015f olan Nanhua Xiafang Formasyonu, Shabahuang Formasyonu, Hongshan Formasyonu, Sinian Laohutang Formasyonu ve Kambriyen Waiguankeng Formasyonu yer al\u0131r. Kuvarsitin SiO2 i\u00e7eri\u011fi 98%'nin \u00fczerindedir. Magma temasl\u0131 termal metamorfizman\u0131n veya baz\u0131 pozitif korelasyonlu tektonik eylemlerin \u00fcst \u00fcste gelmesi nedeniyle kuvars do\u011fal olarak daha fazla safla\u015ft\u0131r\u0131labilir. Kuvars\u0131n i\u00e7inde \u00e7ok az gaz-s\u0131v\u0131 kapan\u0131m\u0131 vard\u0131r ve SiO2 i\u00e7eri\u011fi 99%'nin \u00fczerine \u00e7\u0131kar. \u00d6n de\u011ferlendirmeye g\u00f6re, y\u00fcksek kaliteli ve y\u00fcksek safl\u0131kta kuvars hammaddesi olma potansiyeline sahiptir.<\/p>\n\n\n\n

\"\"<\/figure>\n\n\n\n

Geli\u015ftirme ve kullan\u0131m \u00f6nerileri<\/h2>\n\n\n\n

(1) Jiangxi'nin kuvars y\u00fcksek teknoloji end\u00fcstrisinin uygulama durumunu anlamak i\u00e7in farkl\u0131 kuvars kaynaklar\u0131n\u0131n geli\u015ftirilmesi ve kullan\u0131m\u0131 konusunda ara\u015ft\u0131rma yap\u0131lmas\u0131 \u00f6nerilir.<\/h3>\n\n\n\n

Sosyal ekonominin, bilim ve teknolojinin h\u0131zla geli\u015fmesiyle birlikte, geleneksel end\u00fcstrilerde kuvars kaynaklar\u0131na olan talebin istikrarl\u0131 bir \u015fekilde artmas\u0131n\u0131n yan\u0131 s\u0131ra, yar\u0131 iletken, fotovoltaik ve ileti\u015fim end\u00fcstrileri son derece pop\u00fcler hale gelmi\u015f ve kuvars kaynaklar\u0131na olan talep \u00f6nemli \u00f6l\u00e7\u00fcde artm\u0131\u015ft\u0131r. Ayr\u0131ca, y\u00fcksek kaliteli kuvars kaynaklar\u0131n\u0131n k\u0131tl\u0131\u011f\u0131, \u00fclkemde yetersiz genel \u00fcretim kapasitesine ve s\u0131n\u0131rl\u0131 kuvars kayna\u011f\u0131 arz\u0131na neden olmu\u015ftur. \u00d6te yandan, y\u00fcksek teknoloji alan\u0131 kuvars safl\u0131\u011f\u0131 i\u00e7in giderek daha y\u00fcksek gereksinimlere sahiptir. Y\u00fcksek safl\u0131kta kuvars, baz\u0131 b\u00fcy\u00fck \u00fclkeler ve g\u00fc\u00e7ler taraf\u0131ndan stratejik bir kaynak olarak listelenmi\u015ftir (Guo Jia, 2018; Chen Qishen, 2021) ve orta ve y\u00fcksek kaliteli y\u00fcksek safl\u0131kta kuvars kumunun \u00fcretim teknolojisi, \u00e7e\u015fitli \u00fclkelerin h\u00fck\u00fcmetleri taraf\u0131ndan y\u00fcksek teknoloji alan\u0131na dahil edilmi\u015ftir ve s\u0131k\u0131 bir \u015fekilde korunmaktad\u0131r. Jiangxi, kuvars kaynaklar\u0131 a\u00e7\u0131s\u0131ndan zengindir. Ge\u00e7mi\u015fte, eyalet genelinde kaynaklar ve bunlar\u0131n geli\u015ftirme durumlar\u0131 hakk\u0131nda sistematik bir ara\u015ft\u0131rma ve inceleme yap\u0131lmam\u0131\u015ft\u0131r. Farkl\u0131 kuvars kaynaklar\u0131n\u0131n geli\u015ftirilmesi ve kullan\u0131m\u0131 \u00fczerine ara\u015ft\u0131rmalar yaparak, kaynaklar\u0131n durumunu, geli\u015fimini ve kullan\u0131m\u0131n\u0131 anlayabilir, \u00f6zellikle kuvars mineral hammaddelerinin kalitesini, end\u00fcstriyel zincirinin geni\u015fletilmesini ve y\u00fcksek teknoloji end\u00fcstrilerindeki uygulamalar\u0131 analiz edebilir, Jiangxi'nin y\u00fcksek teknoloji end\u00fcstrilerinin ve ilgili end\u00fcstriyel kalk\u0131nma planlar\u0131n\u0131n geli\u015ftirilmesi i\u00e7in teknik destek sa\u011flayabiliriz.<\/p>\n\n\n\n

<\/p>\n\n\n\n

(2) Y\u00fcksek safl\u0131kta kuvars silisli hammaddelerin eyaletin temel ke\u015fif minerallerine dahil edilmesi tavsiye edilir ve Jiangxi'nin geli\u015fmekte olan end\u00fcstrilerinin h\u0131zla geli\u015fmesi i\u00e7in kaynak garantileri sa\u011flamak amac\u0131yla arama ve bilimsel ara\u015ft\u0131rmalar\u0131n art\u0131r\u0131lmas\u0131 y\u00f6n\u00fcnde \u00e7aba g\u00f6sterilmelidir.<\/h3>\n\n\n\n

Y\u00fcksek safl\u0131kta kuvars, \u00fcst d\u00fczey teknoloji alan\u0131nda temel bir hammaddedir. \u00c7ip g\u00fcvenli\u011fini, optik fiber g\u00fcvenli\u011fini, fotovoltaik g\u00fcvenli\u011fi ve \u00fcst d\u00fczey cihaz g\u00fcvenli\u011fini sa\u011flamak i\u00e7in ulusal stratejik \u00f6neme sahiptir. 7 Kas\u0131m 2018'de Ulusal \u0130statistik B\u00fcrosu, y\u00fcksek safl\u0131kta kuvars\u0131 ilk kez ulusal stratejik kaynaklar seviyesine y\u00fckselten "Stratejik Ortaya \u00c7\u0131kan End\u00fcstrilerin S\u0131n\u0131fland\u0131rmas\u0131 (2018)"ni yay\u0131nlad\u0131. \u201cJiangxi Eyaletinin Ulusal Ekonomik ve Sosyal Kalk\u0131nmas\u0131 i\u00e7in 14. Be\u015f Y\u0131ll\u0131k Plan\u0131n Ana Hatlar\u0131 ve 2035 Uzun Vadeli Hedefleri\u201d, end\u00fcstriyel g\u00fc\u00e7lendirme stratejisinin derinle\u015ftirilmesi, havac\u0131l\u0131k, elektronik bilgi, ekipman imalat\u0131, geleneksel \u00c7in t\u0131bb\u0131, yeni enerji ve avantajlara dayal\u0131 yeni malzemeler gibi geli\u015fmekte olan end\u00fcstrilere odaklan\u0131lmas\u0131, end\u00fcstrinin \u201c2+6+N\u201d y\u00fcksek kaliteli s\u0131\u00e7ramal\u0131 geli\u015ftirme eyleminin g\u00fc\u00e7l\u00fc bir \u015fekilde uygulanmas\u0131, end\u00fcstriyel taban\u0131 y\u00fckseltme ve end\u00fcstriyel zinciri modernize etme m\u00fccadelesine kararl\u0131l\u0131kla kar\u015f\u0131 konulmas\u0131 ve geleneksel end\u00fcstrilerin d\u00f6n\u00fc\u015ft\u00fcr\u00fclmesi ve y\u00fckseltilmesi ve \u00fclkedeki geli\u015fmekte olan end\u00fcstrilerin yeti\u015ftirilmesi ve geli\u015ftirilmesi i\u00e7in bir yayla yarat\u0131lmas\u0131 gerekti\u011fini belirtti. Jiangxi'de elektronik bilgi (bask\u0131l\u0131 devre kartlar\u0131, optoelektronik ekranlar, yar\u0131 iletken ayd\u0131nlatma), yeni enerji (fotovoltaik) ve yeni malzemeler (yar\u0131 iletken yeni malzemeler) gibi end\u00fcstrilerin yo\u011fun geli\u015fimiyle birlikte, y\u00fcksek safl\u0131ktaki kuvars talebi s\u00fcrekli bir b\u00fcy\u00fcme e\u011filimi g\u00f6stermektedir. Kaynak sorunu \u00e7\u00f6z\u00fclemezse, ithalata ba\u011f\u0131ml\u0131l\u0131k derecesi artmaya devam edecektir. Jiangxi'de y\u00fcksek teknoloji end\u00fcstrileri i\u00e7in yeni b\u00fcy\u00fcme noktalar\u0131n\u0131 daha iyi yeti\u015ftirmek ve y\u00fcksek kaliteli ekonomik kalk\u0131nmay\u0131 te\u015fvik etmek i\u00e7in, eyaletin temel ke\u015fif minerallerine y\u00fcksek safl\u0131kta kuvars i\u00e7in silisli hammaddelerin dahil edilmesi, finansal yat\u0131r\u0131m\u0131n art\u0131r\u0131lmas\u0131, sosyal yat\u0131r\u0131ma rehberlik edilmesi, kaynak ara\u015ft\u0131rmas\u0131 ve de\u011ferlendirmesi, mineral i\u015fleme ve ar\u0131tma gibi temel teknoloji ara\u015ft\u0131rma ve geli\u015ftirmelerini y\u00fcr\u00fctmek \u00fczere jeolojik ara\u015ft\u0131rma birimlerinin ve bilimsel ara\u015ft\u0131rma enstit\u00fclerinin te\u015fvik edilmesi ve desteklenmesi, yukar\u0131 ve orta ak\u0131\u015f end\u00fcstrilerinin eksikliklerinin giderilmesi ve y\u00fcksek safl\u0131kta kuvars\u0131n kullan\u0131m\u0131 i\u00e7in tam bir end\u00fcstriyel zincir olu\u015fturulmas\u0131 \u00f6nerilir.<\/p>\n\n\n\n

<\/p>\n\n\n\n

(3) Y\u00fcksek kaliteli kuvars kaynaklar\u0131n\u0131n bilimsel ve verimli kullan\u0131m\u0131n\u0131 te\u015fvik etmek amac\u0131yla kuvars hammaddeleri i\u00e7in bir s\u0131n\u0131fland\u0131rma ve derecelendirme de\u011ferlendirme y\u00f6ntemi olu\u015fturulmas\u0131 \u00f6nerilmektedir.<\/h3>\n\n\n\n

Kuvars, yaln\u0131zca b\u00fcy\u00fck hacimli t\u00fcketime sahip metalik olmayan bir mineral de\u011fil, ayn\u0131 zamanda y\u00fcksek teknoloji i\u00e7in acilen ihtiya\u00e7 duyulan bir mineraldir. Jiangxi kuvars kaynaklar\u0131n\u0131n geli\u015ftirilmesi ve kullan\u0131m\u0131, y\u00fcksek kaliteli kaynaklar\u0131n d\u00fc\u015f\u00fck kalitede kullan\u0131m\u0131 ve bunun sonucunda y\u00fcksek kaliteli kuvars kaynaklar\u0131n\u0131n kayb\u0131 ve israf\u0131 gibi belirgin bir soruna sahiptir. Bunun ba\u015fl\u0131ca nedeni, kuvars hammaddelerinin de\u011ferlendirilmesi ve uygulama ara\u015ft\u0131rmalar\u0131n\u0131n yeterince derinlemesine olmamas\u0131d\u0131r. Bu nedenle, kuvars hammaddelerinin kapsaml\u0131 bir de\u011ferlendirmesinin yap\u0131lmas\u0131 \u00e7ok \u00f6nemlidir. Jiangxi'deki ana kuvars hammaddeleri \u00fczerinde uygulama alan\u0131na g\u00f6re uygulama uyarlanabilirlik ara\u015ft\u0131rmas\u0131 yap\u0131lmas\u0131 ve kaynaklar\u0131n hiyerar\u015fik geli\u015fimini ve bilimsel kullan\u0131m\u0131n\u0131 kolayla\u015ft\u0131rmak i\u00e7in bir hammadde s\u0131n\u0131fland\u0131rmas\u0131 ve derecelendirme de\u011ferlendirme y\u00f6ntemi olu\u015fturulmas\u0131 \u00f6nerilir. Y\u00fcksek kaliteli kaynaklar\u0131 koruyun ve y\u00fcksek teknoloji alan\u0131nda y\u00fcksek safl\u0131kta kuvars hammaddelerine olan talebi sa\u011flay\u0131n.<\/p>\n\n\n\n

<\/p>\n\n\n\n

(4) End\u00fcstriyel geli\u015fmeyi te\u015fvik etmek amac\u0131yla konum ve kaynak avantajlar\u0131na dayal\u0131 bir kuvars kaynak geli\u015ftirme ve kullan\u0131m taban\u0131 olu\u015fturulmas\u0131 \u00f6nerilmektedir.<\/h3>\n\n\n\n

Jiangxi, olu\u015fum t\u00fcrlerine g\u00f6re nispeten yo\u011funla\u015fm\u0131\u015f kuvars kaynaklar\u0131 a\u00e7\u0131s\u0131ndan zengindir. Baz\u0131 b\u00f6lgelerde bol miktarda b\u00fcy\u00fck \u00f6l\u00e7ekli, y\u00fcksek kaliteli y\u00fcksek safl\u0131kta kuvars hammaddeleri bulunur. Yerel y\u00f6netimlerin kuvars kaynak geli\u015ftirme ve kullan\u0131m tabanlar\u0131n\u0131 kurmak i\u00e7in kaynak avantajlar\u0131na g\u00fcvenmeleri; kaynak tahsisini daha da optimize etmeleri, tercihli politikalar form\u00fcle etmeleri, modern y\u00fcksek standartl\u0131 kuvars end\u00fcstri parklar\u0131 in\u015fa etmeleri, fabrika in\u015faat\u0131na yat\u0131r\u0131m yapmak i\u00e7in sosyal sermaye \u00e7ekmeleri, kuvars end\u00fcstrisinin toplanmas\u0131n\u0131 ve geli\u015fimini g\u00fc\u00e7l\u00fc bir \u015fekilde te\u015fvik etmeleri ve y\u00fcksek safl\u0131kta kuvars end\u00fcstriyel taban\u0131 olu\u015fturmalar\u0131 \u00f6nerilir.<\/p>\n\n\n\n

<\/p>\n\n\n\n

\u00c7\u00f6z\u00fcm<\/h2>\n\n\n\n

Jiangxi'deki kuvars kaynaklar\u0131 \u00e7e\u015fitli tiplerdedir, yayg\u0131n olarak da\u011f\u0131lm\u0131\u015ft\u0131r ve b\u00fcy\u00fck rezervlere sahiptir. Bunlar aras\u0131nda toz kuvars ve damar kuvars avantajl\u0131 minerallerdir ve kaynak rezervleri \u00fclkede ilk s\u0131rada yer almaktad\u0131r. Kuvars t\u00fcr\u00fc end\u00fcstriyel uygulamay\u0131 belirler. Kuvarsit, kuvars kumta\u015f\u0131 ve damar kuvars \u00f6nemli cam hammaddeleridir. Toz kuvars ve damar kuvars, silikon mikro tozu i\u00e7in ana hammaddelerdir. Granit kuvars ve kuvarsit, elveri\u015fli y\u00fcksek safl\u0131kta kuvars hammaddeleridir. Jiangxi'deki kuvars kaynaklar\u0131n\u0131n geli\u015ftirilmesi ve kullan\u0131m\u0131n\u0131n mevcut durumu ve mevcut sorunlar\u0131 g\u00f6z \u00f6n\u00fcnde bulunduruldu\u011funda, d\u00f6rt \u00f6neri \u00f6ne s\u00fcr\u00fclmektedir: 1) Jiangxi'deki kuvars y\u00fcksek teknoloji end\u00fcstrilerinin uygulamas\u0131n\u0131 bulmak i\u00e7in farkl\u0131 tipteki kuvars kaynaklar\u0131n\u0131n geli\u015ftirilmesi ve kullan\u0131m\u0131 konusunda bir ara\u015ft\u0131rma yap\u0131lmas\u0131 \u00f6nerilir; 2) Eyaletin temel ke\u015fif minerallerine y\u00fcksek safl\u0131kta kuvars i\u00e7in silisli hammaddelerin dahil edilmesi, arama ve bilimsel ara\u015ft\u0131rma yo\u011funlu\u011funun art\u0131r\u0131lmas\u0131 ve Jiangxi'deki yeni ortaya \u00e7\u0131kan end\u00fcstrilerin h\u0131zl\u0131 geli\u015fimi i\u00e7in kaynak garantilerinin sa\u011flanmas\u0131 \u00f6nerilir; 3) Y\u00fcksek kaliteli kuvars kaynaklar\u0131n\u0131n bilimsel ve verimli kullan\u0131m\u0131n\u0131 te\u015fvik etmek amac\u0131yla kuvars hammaddeleri i\u00e7in bir s\u0131n\u0131fland\u0131rma ve derecelendirme de\u011ferlendirme y\u00f6ntemi olu\u015fturulmas\u0131 \u00f6nerilmektedir; 4) End\u00fcstriyel geli\u015fimi te\u015fvik etmek amac\u0131yla konum ve kaynak avantajlar\u0131na dayal\u0131 bir kuvars kaynak geli\u015ftirme ve kullan\u0131m taban\u0131 olu\u015fturulmas\u0131 \u00f6nerilmektedir.<\/p>\n\n\n\n

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