...
首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Multiple proxies indicating methane seepage as the origin of Devonian large barite deposit in Zhenning-Ziyun, Guizhou, SW China
【24h】

Multiple proxies indicating methane seepage as the origin of Devonian large barite deposit in Zhenning-Ziyun, Guizhou, SW China

机译:中国西南部贵宁市紫云泥盆纪大型重晶石矿床的成因表明甲烷渗透

获取原文
获取原文并翻译 | 示例
           

摘要

Bedded barite deposits are found in Cambrian and Devonian strata in China. In this paper, we report the occurrence of Late Paleozoic methane seeps from bedded barite in one of the largest barite deposits in China. The ore bodies are stratiform and lenticular in shape and are hosted within Upper Devonian cherts. The barite deposits usually have laminar, banded, fragmental, massive and rosette textures, and radial and spheroidal structures were observed in the barite ores. Nodular limestones are associated with the barite deposits; they consist of clotted micrites and framboidal pyrites. The internal structure of framboidal pyrite is simple, in which the sun-flower structure has been observed, similar to modern seep carbonates. The delta C-13(V-PDB) values range from -8.82 parts per thousand to -10.27 parts per thousand, and delta O-18(V-PVB) ranges from -8.10%. to -8.20%. in Xiyahe and from +0.03 parts per thousand to -3.31%. in Luocheng. The C-13 depletion suggests that these carbonates formed in a methane seep through the anaerobic oxidation of methane (ADM). This evidence lends strong support to the interpretation that methane hydrate contributed to the barite deposition. In addition, the delta C-13(V-PDB) values decrease, gradually from Xiyahe to Luocheng, which indicates the gradually weakening strength of the methane seep activities. The delta Si-30(NBS-28) values of the cherts range from -0.3 parts per thousand to +0.5 parts per thousand, except for two samples (LJ-24: delta Si-30(NBS-28) values = +0.9 parts per thousand; ZL18: delta Si-30(NBS-28) values = +1.1 parts per thousand). The lowest delta Si-30(NBS-28) values reflect silicon derived from hydrothermal fluids ascribed to intense tectonic activity, which consequently caused the rapid maturity of hydrocarbons. The Sr-87/Sr-86 values (Sr-87/Sr-86 = 0.70863-0.70898, avg. 0.70877; n = 11) of barite are higher than the average value of contemporary seawater, showing that hydrothermal processes played a minor role in barite mineralization. (C) 2016 Elsevier B.V. All rights reserved.
机译:在中国的寒武纪和泥盆纪地层中发现了层状重晶石矿床。在本文中,我们报道了中国最大的重晶石矿床之一中,由层状重晶石引起的晚古生代甲烷渗漏的发生。矿体呈层状和双凸状,并存在于上泥盆统石中。重晶石矿床通常具有层状,带状,碎片状,块状和玫瑰状结构,并且在重晶石矿石中观察到放射状和球状结构。球状灰岩与重晶石沉积有关。它们由凝结的微尘和黄铁矿黄铁矿组成。黄菊黄铁矿的内部结构很简单,其中观察到了向日葵的结构,类似于现代的渗碳碳酸盐。 ΔC-13(V-PDB)值的范围为-8.82千分之几至-10.27千分之十,ΔO-18(V-PVB)范围为-8.10%。至-8.20%。 Xiyahe中的百分含量从+0.03到-3.31%。在罗城C-13消耗表明这些碳酸盐是通过甲烷的厌氧氧化(ADM)在甲烷中形成的。该证据为甲烷水合物促成重晶石沉积的解释提供了有力的支持。此外,δC-13(V-PDB)值从西河河到洛城逐渐减小,表明甲烷渗流活动的强度逐渐减弱。 two石的δSi-30(NBS-28)值范围从-0.3千分之几至+0.5千分之二(两个样品除外)(LJ-24:δSi-30(NBS-28)值= +0.9千分之几; ZL18:δSi-30(NBS-28)值= +1.1千分之一。最低的Si-30(NBS-28)值反映出归因于强烈构造活动的热液中的硅,从而导致烃类迅速成熟。重晶石的Sr-87 / Sr-86值(Sr-87 / Sr-86 = 0.70863-0.70898,平均0.70877; n = 11)高于当代海水的平均值,表明水热过程的作用较小重晶石矿化。 (C)2016 Elsevier B.V.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号