洛南紫绿玛瑙地质特征及其综合开发利用
Luonan Purple Green Agate Geological Characteristics and Their Comprehensive Exploitation and Utilization
摘要: 紫绿玛瑙为全世界稀缺品种,近年来发现的洛南紫绿玛瑙为21世纪中国宝玉石资源重大发现,其古称紫玉,近代称为洛翠玉,2012年宝玉石界命名为紫绿玛瑙,因其产于华山南麓,亦称华阳玉,为中国目前紫绿玛瑙唯一产地。其质地温润坚毅,色彩饱和浓艳,色调丰富,色差截然,层次分明,组合多样,可雕性好,资源稀缺受到市场追捧,业界学者将紫绿玛瑙列为市场新贵,与翡翠、和田玉、南红玛瑙并称四大国玉,有“九色之首,百玉之尊”雅称。研究认为其产出层位为长城系杜关组上段下部原划紫红色、灰绿色泥岩,厚约5~17米,实际为一套同生沉积火山碎屑岩、沉凝灰岩。玛瑙产出层位受该层火山岩控制;矿带展布受白花岭–路家街复向斜之路家街复向斜南北两翼控制;其宝玉石资源分类为石英岩玉及蚀变白云岩玉大类。文章提出紫绿玛瑙定义,对赋矿地层杜关组进行厘定,探讨了地质特征、成因、资源分类,结合市场走势,对其品级进行分类。提出综合开发构想,认为只有采用不同流派的雕工艺术,将紫绿玛瑙稀缺性赋予深厚的洛南文化、中华文化元素,才能实现价值最大化;只有综合开发利用,多元化产业发展,才能实现美丽农村建设,以稀缺资源助推地方经济腾飞。对紫绿玛瑙相关资源规划、勘查,产业布局,商业开发、原料采购、文玩收藏、鉴赏等均有借鉴意义。
Abstract: The purple and green agate is a rare species in the world. In recent years, the discovery of the purple and green agate of Luonan is a major discovery of treasure jade stone in China in the 21st century. Its ancient name is purple jade. In modern times it is called Luocui jade, and in 2012 treasure jade stone world named it as the purple and green agate. Because it is produced in the south foot of Huashan, it is also known as Huayang agate. Its material properties can be described as warm and firm; the color saturation is gaudy, rich in tone, chromatic aberration is distinct, the combination is diversiform, and it can be easily carved. Because of its scarce resource, the scholars of the industry listed the purple and green agate as the new aristocracy of the market; it is known as one of the four major jades of China along with jade, Hetian jade and southern red agate, and it is called “The head of the nine colors, the honor of all the jades”. According to the research, the output layer is the original purplish red and lime-green mudstone on the bottom of the upper part of the Duguan group in the Great Wall series, which is about 5 - 17 meters thick, and it is actually a set of syngenetic sedimentary pyroclastic and sedimentary limestone. The level of agate output layer is controlled by the volcanic rock. The mine strip is controlled by the north and south wing of the road homing street in the street of the white flower-road. Its treasure jade stone resources are classified as quartzite jade and the alteration of dolomite. The article puts forward the definition of agate, and discusses the geological characteristics, causes, resource classification and the classification of the grade in the mineralization stratum. The concept of comprehensive development is put forward, and it is thought that only by adopting the art of carving of different schools and making the purple and green agate scarcity to the deep Luonan culture and Chinese cultural elements can the value maximization be realized. Only by comprehensive development and utilization, and diversified industrial development can the construction of beautiful countryside be realized, and can the local economy be boosted by scarce resources. It can be used for reference for the planning, exploration, industrial layout, commercial development, raw material purchasing, art collection and appreciation.
文章引用:张锋军, 杜少喜, 王淼, 杨运军. 洛南紫绿玛瑙地质特征及其综合开发利用[J]. 地球科学前沿, 2017, 7(4): 513-525. https://doi.org/10.12677/AG.2017.74053

参考文献

[1] 马润华, 伊鹍英, 王振东, 等. 陕西省岩石地层[M]. 武汉: 中国地质大学出版社, 1998, 第一版: 13-25.
[2] 韩芳林, 张栓厚, 董王仓, 等.陕西省区域地质志[M]. 终审稿,陕西省地质调查院,2012: 39-45.
[3] 张国伟, 张本仁, 等. 秦岭造山带与大陆动力学[M]. 北京: 科学出版社, 2001.
[4] 杨宗让. 秦岭造山带及邻区中晚元古宙板块构造与成矿作用初析[J]. 陕西地质, 2003(3): 1-8.
[5] 王继辉, 徐涛, 毛归来, 等. 陕西省华阴–商州有色金属远景调查报告[R]. 西安: 陕西省地质调查院, 2015: 11-15.
[6] 李诺, 陈衍景, 张辉, 等. 东秦岭斑岩钼矿带的地质特征和成矿构造背景[J]. 地学前缘, 2007, 14(27): 186-198.
[7] Zhang, F.J., Yang, Y.J. and Lu, S.X. (2014) Molybdenum Polymetallic Metallogenic Regularity and Metallogenic Prediction of the Jinduicheng-Huang Longpu Mineral Field, Shanxi Provice. Acta Geologica Sinica (English Edition), 88, 647-648.
[8] 李六全. 陕西黄龙铺–河南栾川地区钼矿床地质特征及控矿因素[J]. 陕西地质, 2008, 26(2): 9-32.
[9] 武清周, 王鼎夏, 等. 石家湾钼矿床围岩蚀变特征及与成矿的关系[M]//陕西秦巴地质论文稿集(一). 西安: 陕西地质矿产局编, 1985: 40-50.
[10] 中国地质科学院成矿远景区划室. 矿床成矿模式选编(二) [M]. 北京: 中国地质科学院, 1991.
[11] 左志东, 等. 1:5万石门幅地质图及区域地质调查报告[M]. 西安: 陕西省地矿局第六地质队, 1989.
[12] 陕西秦巴地质论文稿集(一) [M]. 西安: 陕西地质矿产局编, 1985: 137-155.
[13] 沙丁茂. 陕西小秦岭区域地球化学特征探讨[M]//陕西秦巴地质论文稿集(一). 西安: 陕西地质矿产局编, 1985: 187-194.
[14] 奥和会, 张恒武, 解俊玉, 等. 陕西小秦岭钼矿的控矿条件遥感地质研究及成矿定量预测[M]//陕西秦巴地质论文稿集(一). 西安: 陕西地质矿产局编, 1985: 137-155.
[15] 李永峰, 毛景文, 胡华斌, 等. 东秦岭钼矿类型、特征、成矿时代及其地球动力学背景[J]. 矿床地质, 2005, 24(3): 292-304.
[16] 严芳玲. 金堆城钼矿床中铅的分布规律及赋存特征研究[J]. 有色金属, 2007, 59(2): 265-281.
[17] 许成, 宋文磊, 漆亮. 黄龙铺钼矿田含矿碳酸岩地球化学特征及其形成构造背景[J]. 岩石学报, 2009, 29(2): 422-429.
[18] 樊益民, 周依磐, 李伯平. 陕西洛南石坡–黄龙铺钼地区小岩体分类及其岩浆演化[J]. 陕西地质科技情报, 1983(9): 22-27.
[19] 胡明安, 低温成矿系列中生物有机质的矿床学意义[J]. 地球科学, 2000(4): 375-379.
[20] 吴向东, 樊益民, 薛祖雷. 陕西金堆城地区含矿花岗岩类的地球化学特征探讨[M]//陕西秦巴地质论文稿集(一). 西安: 陕西地质矿产局编, 1985: 51-61.
[21] 沙丁茂. 陕西小秦岭区域地球化学特征探讨[M]//陕西秦巴地质论文稿集(一). 陕西地质矿产局编, 1985年: 187-194.
[22] 孙红杰. 东秦岭钼矿的主要类型和成矿时代浅析[J]. 矿床地质, 2009, 28(3): 28-33.
[23] 田战武, 韩俊民, 潘振兴, 等. 小秦岭地区钼矿类型、地质特征及控矿因素[J]. 内蒙古石油化工, 2007(1): 92-94.
[24] 李厚民, 叶会寿, 毛景文, 等. 小秦岭金(钼)矿床辉钼矿铼一锇定年及其地质意义[J]. 矿床地质, 2007, 26(4): 417-424.
[25] 周国平. 宝石学[M]. 武汉: 中国地质大学出版社, 1998.
[26] 郭守国. 宝玉石学教程[M]. 北京: 科学出版社, 1998.
[27] 张锋军, 李文佳. 商洛市萤石矿资源及其综合开发利用[J]. 陕西地质, 2008, 26(1): 52-56.
[28] 李铁, 李进学, 李梦疑, 等. 秦岭终南山地质公园地质遗迹保护与旅游资源开发[J]. 陕西地质, 2009, 26(1): 103-108.