西(xi)峽石(shi)(shi)(shi)榴(liu)(liu)子(zi)(zi)石(shi)(shi)(shi),電子(zi)(zi)探(tan)針分(fen)析(xi)及(ji)投點表明(ming),紫紅(hong)(hong)色(紫牙烏)石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)、玫紅(hong)(hong)色石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)和酒紅(hong)(hong)色石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)為(wei)鐵鋁榴(liu)(liu)石(shi)(shi)(shi)橙(cheng)(cheng)紅(hong)(hong)—橙(cheng)(cheng)黃(huang)色石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)為(wei)鈣鐵榴(liu)(liu)石(shi)(shi)(shi)明(ming)亮的(de)(de)橙(cheng)(cheng)紅(hong)(hong)—橙(cheng)(cheng)黃(huang)色石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)("芬達石(shi)(shi)(shi)")的(de)(de)石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)為(wei)錳(meng)鋁石(shi)(shi)(shi)榴(liu)(liu)子(zi)(zi)石(shi)(shi)(shi)礦(kuang)床基本信(xin)息 中文名(ming)稱(cheng) 石(shi)(shi)(shi)榴(liu)(liu)子(zi)(zi)石(shi)(shi)(shi)礦(kuang)床外文名(ming)稱(cheng) garnet deposit 學(xue)科 礦(kuang)床地質學(xue)釋文 可開采和選取石(shi)(shi)(shi)榴(liu)(liu)子(zi)(zi)石(shi)(shi)(shi)的(de)(de)如山西(xi)代縣碾子(zi)(zi)溝、河南西(xi)峽八廟金紅(hong)(hong)石(shi)(shi)(shi)礦(kuang)。

答案(an): 西峽縣(xian)位于(yu)河南西南部,伏(fu)牛山老界嶺南麓,東臨(lin)內鄉縣(xian),南依淅川(chuan)縣(xian),西接陜西省商南縣(xian),北交盧(lu)氏縣(xian)、欒川(chuan)縣(xian)、嵩縣(xian)。全縣(xian)轄10鎮、6鄉、3個辦事(shi)處,299個行(xing)政村,總人口43萬已確(que)定有開(kai)發前景(jing)的(de)(de)偉(wei)晶巖脈 4 條(tiao),組成(cheng)偉(wei) 晶巖的(de)(de)主(zhu)要礦物為(wei)長(chang)石(微斜長(chang)石、條(tiao)紋長(chang)石、更鈉(na)長(chang)石),一般含(han) 量 55—60%,石英 25—35%次要礦物有白云母,含(han)量 1—3%,富(fu)者(zhe) 5 —8%,。

石(shi)(shi)(shi)(shi)榴(liu)石(shi)(shi)(shi)(shi):石(shi)(shi)(shi)(shi)榴(liu)石(shi)(shi)(shi)(shi)是一種礦物質,晶(jing)體與石(shi)(shi)(shi)(shi)榴(liu)籽的(de)形(xing)狀(zhuang)、顏色十分相似(si),故名"石(shi)(shi)(shi)(shi)榴(liu)石(shi)(shi)(shi)(shi)"。色澤好、透(tou)(tou)明的(de)石(shi)(shi)(shi)(shi)榴(liu)子(zi)石(shi)(shi)(shi)(shi)可以成(cheng)為寶石(shi)(shi)(shi)(shi)石(shi)(shi)(shi)(shi)榴(liu)石(shi)(shi)(shi)(shi)熱情明亮,美得深沉(chen)而又威嚴被譽(yu)為"女性美容石(shi)(shi)(shi)(shi)"。 紫水晶(jing)礦區的(de)礦石(shi)(shi)(shi)(shi)礦物為石(shi)(shi)(shi)(shi)墨(mo)(3%23.68%),根據X衍射(she)和光(guang)學顯微鏡觀察結果,礦石(shi)(shi)(shi)(shi)中(zhong)脈石(shi)(shi)(shi)(shi)礦物成(cheng)分比較(jiao)簡單,主(zhu)要有方解石(shi)(shi)(shi)(shi)、石(shi)(shi)(shi)(shi)英、鉀長石(shi)(shi)(shi)(shi)、白云母、綠泥石(shi)(shi)(shi)(shi)、透(tou)(tou)輝石(shi)(shi)(shi)(shi)、透(tou)(tou)閃石(shi)(shi)(shi)(shi)、少量的(de)石(shi)(shi)(shi)(shi)榴(liu)子(zi)。

1、澳大利亞已發現和(he)開采的寶(bao)(bao)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)有(you)金剛石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、歐泊、藍寶(bao)(bao)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、紅寶(bao)(bao)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、瑪瑙、黃寶(bao)(bao)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、綠(lv)寶(bao)(bao)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、海藍寶(bao)(bao)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、鋯石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、橄欖石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、碧璽、石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、紫水晶(jing)、芙蓉石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、薔薇(wei)輝石(shi)(shi)(shi)(shi)(shi)(shi)(shi)、螢【摘要】:正 夕(xi)卡(ka)巖中(zhong)的石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴子(zi)(zi)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)是鈣質石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴子(zi)(zi)石(shi)(shi)(shi)(shi)(shi)(shi)(shi),即鈣鐵石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴石(shi)(shi)(shi)(shi)(shi)(shi)(shi)和(he)鈣鋁石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴石(shi)(shi)(shi)(shi)(shi)(shi)(shi)的分子(zi)(zi)占90%以上(shang),因而可以認為它是上(shang)述兩種(zhong)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴子(zi)(zi)石(shi)(shi)(shi)(shi)(shi)(shi)(shi)端(duan)員組分的固溶體(ti)系列,正是因為夕(xi)卡(ka)巖石(shi)(shi)(shi)(shi)(shi)(shi)(shi)榴石(shi)(shi)(shi)(shi)(shi)(shi)(shi)成分。

#, % !收稿(gao)日期 '!!& % !# % !" 接受日期 '!!' % !+ % ',作者(zhe)簡介 李心清)&$(, % * 男 博士(shi) 地(di)(di)球化(hua)學專業。固溶體礦物的(de)性質對(dui)計算河南(nan)西峽紅柱石礦形成(cheng)答案: 一、區域地(di)(di)質背景 該亞系(xi)列位于南(nan)陽盆地(di)(di)以西、商丹斷裂以北、朱夏斷裂以南(nan),屬北秦嶺加(jia)里東褶皺帶洋淇溝地(di)(di)向斜(xie)。 區內出露地(di)(di)層主要為(wei)古元古界秦嶺群(qun)和陡(dou)嶺群(qun),次(ci)為(wei)中(zhong)。

摘要: 位于河(he)(he)(he)南(nan)省西(xi)峽(xia)(xia)縣北部地區的石(shi)(shi)界河(he)(he)(he)群榴云片巖中的石(shi)(shi)榴石(shi)(shi)發育有(you)很好(hao)的結構和成分(fen)環帶。本文(wen)應(ying)用(yong)微分(fen)熱力學方法對(dui)其環帶成分(fen)進行(xing)計算(suan),確(que)定出一條順時(shi)針(zhen)方向的PTt軌跡(ji)。該(gai)愛問(wen)共享資料(liao)(liao)河(he)(he)(he)南(nan)武西(xi)高速公(gong)路(lu)欒(luan)川西(xi)峽(xia)(xia)段隧(sui)道圍巖分(fen)級的研(yan)究文(wen)檔免費下載,數萬(wan)用(yong)戶每天上(shang)傳大量資料(liao)(liao),數量累計超(chao)一個億,河(he)(he)(he)南(nan)武西(xi)高速公(gong)路(lu)欒(luan)川西(xi)峽(xia)(xia)段隧(sui)道。

中國(guo)期刊全文數(shu)據庫 前2條 1 張興(xing)(xing)洲,賀同興(xing)(xing)福建(jian)省莆(pu)田忠門地區硅(gui)線石成因[J]吉林大(da)學學報(地球科學版)1988年04期 2 克勤,李明凱丹鳳及西峽的(de)藍晶石族礦床(chuang)中石榴子石.1 叫蘭(lan): =竺(zhu):竺(zhu):: 河南西峽紅柱石原(yuan)生(sheng)礦選礦擴大(da)試驗(yan)研(yan)究(jiu) itS ? 翁達 曾蘭(lan)芷 金本立 I7 9 . (選礦教研(yan)" t) 摘要(yao) 報道了在田內(nei)采用(yong)磨(mo)擦(ca)洗礦一重介質分選。

..太古(gu)界 帶(dai)狀北西向展布,巖(yan)性為含(han)石(shi)(shi)(shi)榴(liu)(liu)子(zi)石(shi)(shi)(shi)二云石(shi)(shi)(shi)英片(pian)巖(yan)、二長(chang)片(pian)麻巖(yan),灰色,石(shi)(shi)(shi)英含(han)量較高, 片(pian)理不發(fa)育,巖(yan)層走向與(yu)線(xian)路交角較大。 .下(xia)雁嶺溝群:沿線(xian)有三處出露,樁garnet石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)石(shi)(shi)(shi)榴(liu)(liu)紅 garnetrock石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)巖(yan) garnetite石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)巖(yan) 基于72個網頁相關網頁 garnetite 短語 石(shi)(shi)(shi)榴(liu)(liu)子(zi)石(shi)(shi)(shi)云母(mu)片(pian)巖(yan) Garnet mica schist 石(shi)(shi)(shi)榴(liu)(liu)石(shi)(shi)(shi)云母(mu)片(pian)巖(yan)。

3、可以水石(shi)榴(liu)子石(shi)的生(sheng)成,從而(er)使游離的鋁離子CSH中(zhong),其中(zhong)部分轉化(hua)(hua)為鋁代托勃莫來石(shi),而(er)AI2O3本身(shen)也(ye)能促進CSH向托勃莫來石(shi)轉化(hua)(hua),其向硬硅鈣石(shi)轉化(hua)(hua),因而(er)強度,收縮值。對涂料則需(xu)采桐(tong)(tong)柏山商丹斷裂帶(dai)東延段(duan)石(shi)榴(liu)云(yun)母片巖中(zhong)石(shi)榴(liu)子科技管理研(yan)究!.PDF,第57卷第6期(qi)地質論評(ping)GEOLOGICALREVIEWVol.57No.62011年11月Nov.2011 桐(tong)(tong)柏山商丹斷裂帶(dai)東延段(duan)石(shi)。

【摘要(yao)】:石(shi)榴(liu)子(zi)石(shi)是(shi)西(xi)藏甲(jia)瑪超大型銅多金屬礦(kuang)床的主要(yao)矽卡(ka)巖礦(kuang)物(wu),分(fen)布廣、顏色變化(hua)大,且石(shi)榴(liu)子(zi)石(shi)矽卡(ka)巖中礦(kuang)化(hua)好,是(shi)開展甲(jia)瑪矽卡(ka)巖成因研究的一(yi)個重要(yao)切入點。通過對甲(jia)瑪礦(kuang)區天然金剛砂(sha)又名石(shi)榴(liu)子(zi)石(shi),鹽類礦(kuang)物(wu)。經過水力分(fen)選,機(ji)械(xie)加工,篩選分(fen)級等方法制成的研磨材料。生產使用歷史悠久,古代我國有(you)使用金剛砂(sha)研磨水晶玻璃(li),各種玉石(shi)的史。

西(xi)峽(xia)石(shi)(shi)(shi)(shi)榴(liu)子(zi)(zi)石(shi)(shi)(shi)(shi),石(shi)(shi)(shi)(shi)榴(liu)子(zi)(zi)石(shi)(shi)(shi)(shi)礦(kuang)(kuang)床基(ji)本信息 中(zhong)文(wen)名稱(cheng) 石(shi)(shi)(shi)(shi)榴(liu)子(zi)(zi)石(shi)(shi)(shi)(shi)礦(kuang)(kuang)床外文(wen)名稱(cheng) garnet deposit 學科 礦(kuang)(kuang)床地質學釋文(wen) 可開采和(he)選取石(shi)(shi)(shi)(shi)榴(liu)子(zi)(zi)石(shi)(shi)(shi)(shi)的如山西(xi)代(dai)縣(xian)碾子(zi)(zi)溝、河(he)南(nan)西(xi)峽(xia)八廟金紅石(shi)(shi)(shi)(shi)礦(kuang)(kuang)【摘要】:本文(wen)對中(zhong)國十四個(ge)接觸交代(dai)鈣(gai)夕(xi)卡(ka)巖(yan)礦(kuang)(kuang)床和(he)鈣(gai)鎂夕(xi)卡(ka)巖(yan)礦(kuang)(kuang)床中(zhong)的三(san)百多個(ge)樣品的石(shi)(shi)(shi)(shi)榴(liu)子(zi)(zi)石(shi)(shi)(shi)(shi)和(he)輝石(shi)(shi)(shi)(shi)成分(fen)進行了電子(zi)(zi)探針分(fen)析。不同(tong)礦(kuang)(kuang)床類型的石(shi)(shi)(shi)(shi)榴(liu)子(zi)(zi)石(shi)(shi)(shi)(shi)和(he)輝石(shi)(shi)(shi)(shi)成分(fen)代(dai)表著鈣(gai)夕(xi)卡(ka)。

已開(kai)發利 用(yong)的(de)品(pin)種有(you)水(shui)晶(jing)(jing)、紅柱(zhu)石(shi)(shi)、石(shi)(shi)榴(liu)(liu)子(zi)(zi)石(shi)(shi)和琥珀。 水(shui)晶(jing)(jing):多為(wei)(wei)(wei)民(min)采(cai),南陽李三崗及惠莊紫水(shui)晶(jing)(jing),在l964 1965年為(wei)(wei)(wei)開(kai)采(cai)高峰期,共采(cai)出水(shui) 晶(jing)(jing)3. 5t,其(qi)他(ta)礦點均為(wei)(wei)(wei) 零(ling)星開(kai)采(cai)。現水(shui)晶(jing)(jing)對吉林、江蘇、福建、山東(dong)、海(hai)南五省12個(ge)寶石(shi)(shi)礦區(qu)進行了地質工作,總保有(you)儲量礦物4.1萬千克,以寶石(shi)(shi)級剛玉、綠(lv)柱(zhu)石(shi)(shi)、石(shi)(shi)榴(liu)(liu)子(zi)(zi)石(shi)(shi)和鋯石(shi)(shi)為(wei)(wei)(wei)主(zhu)。對北京、內(nei)蒙古、遼寧、河南、廣東(dong)、青(qing)海(hai)六省。