Results 11 to 20 of about 91 (71)
Introduction The Zarshuran gold deposit is located in the Takht-e-Soleyman complex, NW Iran. It is formed in the Iman Khan NW-trending anticline (Mehrabi et al., 1999; Samimi, 1992).
Reza Alipoor +2 more
doaj +1 more source
GOLD-JASPEROID MINERALIZATION IN ZONE OF THE SHARTYMSKIY FAULT (SOUTH URALS)
The Shartymskiy Graben was formed at zone of the Shartymskiy Fault in the late collision stage of development of the Southern Urals on the joint of the Western and Eastern Magnitogorsk sub-zone in conditions of variable compression and stretching, and was made with the Lower Carboniferous limestone. Occurrences of gold-bearing metasomatites (jasperoids,
openaire +2 more sources
Gold mineralization of the Arctic Belt of the Russian Far East
The gold ore-bearing potential of the Early Cretaceous Arctic orogenic belt of the Far Eastern Arctic is characterized. The gold mineralization is represented by the Au-quartz vein, Au-sulfide disseminated in folded and crushed zones, Au-Bi (gold-rare ...
Goryachev N. A.
doaj +1 more source
Sedimentary ancient DNA from caves: Challenges and opportunities
Abstract Caves are unique depositional environments that hold great potential for long‐term preservation of DNA due to their typically cool and stable internal climates, buffered from external climate extremes. Bones from caves have long been recognised as an excellent source of ancient DNA, yet the potential for DNA preservation in cave sediments ...
Siobhan Evans +2 more
wiley +1 more source
RED JASPEROIDS FROM THE AREA OF THE UKRAINIAN ANTARCTIC RESEARCH STATION
Red jasper-like rocks from the area of the Akademik Vernadsky Station are known since the time of the first Ukrainian Antarctic expeditions. But until now, all the published information about them was limited to only one brief mention in the abstract of the report by Mytrokhyn and Bakhmutov (2017). This article summarizes all available data about these
O.V. Mytrokhyn +5 more
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Sediment‐hosted disseminated gold mineralization at the Gegalaw deposit in Central Myanmar
The Gegalaw Au deposit is hosted mainly by framboidal pyrite‐rich carbonaceous and calcareous shale of the Eocene Male Formation. The orebodies are silicified breccia occurring along the NE‐trending secondary faults associated with the major N‐trending Sagaing Fault.
June Born Born +6 more
wiley +1 more source
The Shewushan gold deposit, situated in the western extension of Edongnan, marks the westernmost point of the Middle-Lower Yangtze Metallogenic Belt, is an important iron and copper mineralization area in the Middle-Lower Yangtze Metallogenic Belt (MLYB).
Dongyong Lin +9 more
doaj +1 more source
BİR EPİTERMAL CEVHERLEŞMENİN ANATOMİSİ: MUMCU (BALIKESİR-SINDIRGI), İÇ-BATI ANADOLU
Mumcu'daki epitermal cevherleşme, Simav grabenini dik olarak enine kesen "basit transfer fayları" üzerinde, Paleozoyik (?) yaşlı metamorfitler ile Miyosen yaşlı andezitik volkanitier arasında gelişmiştir.
Vedat OYGÜR
doaj
A unique, highly radioactive variety of fluor it emineral has been recorded in the uranium occurrence of El-Missikat sheared granite pluton. In this occurrence, the uranium assumes different forms, including its presence as discrete, visible, secondary ...
Mohamed Fahmy Raslan
doaj
En este trabajo se analiza el origen y las relaciones entre travertinos y jasperoides intercalados en rocas volcaniclásticas jurásicas en el distrito argento-aurífero Manantial Espejo, ubicado en el borde sur-occidental del Macizo del Deseado, provincia ...
Horacio Echeveste
doaj

