The article describes Reza gold deposit of Ugur exploration area located in Geda- bek Ore District the Lesser Caucasus NW Azerbaijan. It is established that main mineralization consists hematite-barite-quartz-kaoline veins- veinlets and breccia, pyrite stock-stockverk quartz-sulfide veins. On orebody surface center secondary quartzites with vein-veinlets barite-hematite have occured over...

The Golden Ridge gold deposit is located in southwestern New Brunswick, the Canadian Appalachians. Gold mineralization consistently associated with acicular arsenopyrite, and to a lesser degree pyrite, disseminated host rocks, sulphide veinlets, quartz-carbonate veins, breccia matrix. According petrographic-based textural differences, four types of pyrite two arsenopyrite are recognized assembl...

The productive mineralization of the Sheikhdzheili-Zengiboba area is associated with metamorphogenic transformations rocks Urusai, Karauzyak, Kuyanchik, Sheikhdzheili suites, metamorphosed under conditions green schist facies. mineralized zones site are confined to narrow faults in tectonic northeast and northwest directions. main form manifestation gold-bearing small steeply dipping veins, len...

In this paper, we present an algorithm for partitioning any given 2d domain into regions suitable for quadrilateral meshing. It can deal with multi-domain geometries with ease, and is able to preserve the symmetry of the domain. Moreover, this method keeps the number of singularities at the junctions of the regions to a minimum. Each part of the domain, being four-sided, can then be meshed usin...

A common view of the thermal and shock histories of ordinary-chondrite (OC) parent bodies is that, for the most part, thermal and shock metamorphism were distinguishable and successive events; e.g., the decay of 26 Al heated chon-dritic planetesimals and subsequent impacts produced various shock effects. Although collisions have long been acknowledged as capable of producing significant heating...

The Narusongduo Pb-Zn deposit is located at the northern boundary of Luobadui-Milashan fault zone (LMF) in central Tibet and spatially associated with Linzizong volcanic succession (LVS). Our study indicates that regional structural setting was formed by two-stage tectonic events. first stage, spanning from late Mesozoic to early Paleocene, characterized significant N-S crustal shortening Cordi...