共查询到20条相似文献，搜索用时 46 毫秒
1.
2.
3.
4.
通过对喀拉通克矿区1号和2号岩体中铜镍硫化物矿石的Re_Os同位素测年,获得两个等时线年龄数据分别为282.5±4.8Ma和290.2±6.9Ma,187Os/188Os初始比值分别为0.2563±0.0037和0.2721±0.0053,γOs值分别为202.23～1061.59和195.07～473.24,平均值分别为495.05和289.83。上述结果表明成岩成矿年龄极为接近,均介于石炭纪末至早二叠世之间,并且在成矿和岩浆侵位过程中有大量地壳物质混入成岩成矿系统。喀拉通克镁铁质超镁铁质岩带形成于后碰撞的伸展构造环境。 相似文献
5.
新疆哈密月牙湾铜镍矿是近年来在东天山卡拉塔格地区新发现的岩浆型铜镍硫化物矿床.为确定该矿床的成岩、成矿时代及其成矿作用，利用锆石LA-ICP-MS U-Pb定年和硫化物Re-Os同位素等时线定年方法，分别对主含矿岩相橄榄辉长岩和矿石中的磁黄铁矿进行了年龄测定.橄榄辉长岩中锆石的206Pb/238U年龄为255~292 Ma，加权平均值为274±2.4 Ma，代表了橄榄辉长岩的成岩年龄；矿石中磁黄铁矿Re-Os同位素等时线年龄为271.9±9.5 Ma，代表了硫化物熔离成矿的年龄；187Os/188Os初始值为0.279 6±0.008 9，γOs值为117~126，指示在岩浆侵位及硫化物熔离成矿过程中有地壳物质加入.月牙湾镁铁质岩浆的成岩、成矿作用发生于早二叠世，与东天山黄山-图拉尔根一带典型铜镍硫化物矿床为同一时期的产物. 相似文献
6.
赤柏松岩浆型铜镍硫化物矿床位于华北克拉通胶辽吉带,含矿镁铁质—超镁铁质岩侵入到鞍山群最下部的四道砬子河组变质岩中;该矿床硫化物矿样品的Os和Re浓度分别为19×10-3~490×10-3和0.47×10-3~13.97×10-3,对这些数据分析得出了一条6点Re-Os等时线年龄为1 885±94 Ma,矿石的初始(187)^Os/(188)^Os 比值为0.80±0.16 (MSWD=0.17),表明矿石为岩浆源,熔体主要由地幔贡献,但在成矿过程及岩浆侵位期间有不少地壳物质混入成岩成矿系统。新的Re-Os年代学结果表明,赤柏松镁铁质—超镁铁质侵入体与铜镍矿床形成于古元古代,而不是前人认为的早白垩世。 相似文献
7.
内蒙古四子王旗小南山铜镍矿床及外围分布几处镁铁质- 超镁铁质岩体，其成因联系及成矿潜力尚不清晰，制约了该地区铜镍硫化物矿床的找矿工作。本文对小南山、土脑包和白音敖包岩体开展了年代学、岩石学及地球化学研究，结果显示，小南山地区存在两类镁铁质- 超镁铁质岩：小南山、土脑包含铜镍硫化物岩体由辉长岩、辉石岩组成，矿物组合以斜长石、单斜辉石为主，含少量斜方辉石和橄榄石，发育次闪石化、滑石化和绿泥石化；而白音敖包辉长岩不含铜镍硫化物，矿物组合以斜长石、单斜辉石为主，发育绿泥石化和钠黝帘石化，白音敖包辉长岩锆石U- Pb年龄为277. 2±7. 3 Ma，与小南山岩体(272. 7±2. 9 Ma)同期。此外，小南山和土脑包辉长岩Mg#值为0. 56～0. 67，m/f值为1. 25～1. 98，MgO与Ni、Co负相关，Ni与Cu/Zr值正相关，稀土元素配分曲线为右倾型；白音敖包辉长岩Mg#值为0. 50～0. 51，m/f值为0. 97～1. 02，MgO与Ni、Co相关性不明显，Cu/Zr值集中在1附近，稀土元素配分曲线为平坦型。岩石地球化学数据指示小南山和土脑包岩体是源自流体交代岩石圈地幔部分熔融，原生岩浆为高镁拉斑玄武质岩浆，岩浆上升过程受到10%～20%陆壳混染，外来硫的加入和分离结晶作用导致硫化物熔离成矿；白音敖包辉长岩由派生岩浆结晶形成，其岩浆源区受到交代作用不明显，岩浆上升过程仅受到5%左右的地壳物质混染，钻探验证没有发现矿体。 相似文献
8.
内蒙古镁铁质-超镁铁质岩型铜镍矿床成矿条件与找矿远景分析 总被引：5，自引：2，他引：5
按构造环境控岩控矿特点,划分区内铜镍型矿成矿(岩)带,分析成矿条件,研究了与该类矿床成矿有关的镁铁质岩、超镁铁质岩分布规律及铜镍硫化物成矿特征,提出了找矿方向和建议. 相似文献
9.
云南白马寨铜镍硫化物矿床Re-Os同位素定年及其地质意义 总被引：10，自引：5，他引：10
采用 Carius 管溶矿、蒸馏法分离 Os、丙酮萃取 Re 和电感耦合等离子体质谱(ICP-MS)联合测定法,对云南白马寨岩浆岩型铜镍硫化物矿硫化物矿石进行了 Re-Os 同位素精确定年,得出其等时线年龄为259±18Ma(MSWD=0.028),~(187)Os/~(188)Os 初始值为0 455±0 024,相当于γ(Os(t)为 263。硫化物矿石 Re/Os 比值为11.56～21.04。研究结果显示,白马寨铜镍硫化物矿床成矿时代与峨眉大火山岩省主喷发期基本同时,其物质来源属壳-幔混合来源,壳源 Os 的加入量约为30%左右。 相似文献
10.
通过对红旗岭铜镍硫化物矿床1号含矿超镁铁质岩体和8号不含矿镁铁-超镁铁质岩体进行单矿物40Ar-39Ar法测年,得到与铜镍硫化物矿床相关的角闪石与黑云母结晶年龄分别为250 Ma和225 Ma,这一结果与前人所报道的K-Ar法年龄有明显的差异.结合与热液矿化相关的斜长伟晶岩锆石SHRIMP法年龄216 Ma,认为镁铁-超镁铁质岩形成于250 Ma左右的印支早期,铜镍硫化物矿床的形成时间晚于含矿岩体,大约为225 Ma前后的印支中期.216 Ma前后的岩浆期后热液叠加对成矿具有积极作用. 相似文献
11.
Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414. 相似文献
12.
13.
Inter-regional correlation of transgressions and regressions in the Cretaceous period 总被引：1，自引：0，他引：1
T. Matsumoto 《Cretaceous Research》1980,1(4):359-373
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous. 相似文献
14.
15.
正1 Introduction Geological studies established on several sections in Lanping-Simao basin have shown that the salt-bearing strata of Mengyejing formation(Yunlong Fm.in Lanping basin)are constituted by an alternation of salt layers and interbedded facies.The latter consists mainly of mudstones,and mudstone-rich conglomerate.The mineralogy and geochemistry of salt-bearing beds and 相似文献
16.
正On 22nd April 2014,with the approach of the 45th World Earth Day,China’s Ministry of Land and resources issued the status of China’s mineral resources in 2013.The first task of the prospecting breakthrough strategy action implemented in the last five years has been completed,and China’s security capacity for mineral resources has been significantly improved.In the 相似文献
17.
正There are more than 700 salt lakes with area of more than 1km2 on the Qinghai-Tibet Plateau of China.In recent years,an oilfield brine was also found in the Nanyishan Section of Qaidam Basin in the Qinghai-Tibet 相似文献
18.
正1 Introduction Physical and numerical models are constructed to investigate the evolution and mechanism of salt migration driven by tectonic processes.In recent years,we have designed and ran series of models to simulate salt 相似文献
19.
YUAN Qin LI Jianguo QIN Zhanjie WEI Haicheng SHENG Shurong SHAN Fashou 《《地质学报》英文版》2014,88(Z1):276-276
正The study of Cretaceous-Palaeogene salt-bearing strata of the Khorat Basin Laos and the Lanping-Simao Basin in Yunnan,China has an great significance not only in explaining the basin evolution and the genesis of potash 相似文献
20.
正Potash is one of the long-term scare deposits in China,and potash prospecting has long been listed as a key brainstorm project for our nation and geological prospecting units.There have been considerable studies in search for potash deposits in the Kuqa depression of the Tarim basin(Jackson et al.,1991;Gemmer et al.,2004;Vendeville,2005;Vendeville and Jackson,1992a,1992b), 相似文献