نتایج جستجو برای: alunite

تعداد نتایج: 143  

1999
F. A. Kruse

1.0 INTRODUCTION Active and fossil hot springs systems occur worldwide, and share many common characteristics that indicate similar genetic histories (White 1955; Waring 1965; Rhinehart 1980; White 1981; Bowen 1989). This research studies the occurrence and characteristics of hot springs at Steamboat Springs, Nevada using Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) data. Both highan...

Abedini, , Ahmadi, , Bagheri, , Calagari, ,

The Baharieh kaolin deposit (east Kashmar, Khorasan Razavi Province) is the product of alteration of dacitic rocks (Eocene) and is located in the Khaf-Kashmar-Bardaskan metallogenic belt. Field observations show that the development of this deposit was controlled by the tectonic system of the area and the presence of silica cap is the most important geological feature of this deposit. Mineralog...

Journal: :Appl. Soft Comput. 2002
Brian J. Ross Anthony G. Gualtieri Frank Fueten Paul Budkewitsch

Genetic programming is used to evolve mineral identification functions for hyperspectral images. The input image set comprises 168 images from different wavelengths ranging from 428 nm (visible blue) to 2507 nm (invisible shortwave in the infrared), taken over Cuprite, Nevada, with the AVIRIS hyperspectral sensor. A composite mineral image indicating the overall reflectance percentage of three ...

Journal: :The Journal of the Society of Chemical Industry, Japan 1962

Journal: :Minerals 2022

Porphyry and epithermal deposits are important sources of base precious metals. Most actively mined have been exhumed such that ore bodies relatively close to the surface therefore locatable economic extract. Identifying characterizing concealed deposits, particularly more deeply buried porphyry represents a far greater challenge for mineral exploration, will become progressively as near-surfac...

Journal: :Chemical Geology 2021

Percolation experiments, using columns filled with alternating layers of hydrated Portland cement and crushed sedimentary rocks, were conducted at PCO2 = 10 bar 60 °C. Limestone, sandstone marl representative reservoir cap rocks for a geologic CO2 storage site. The injected solution was equilibrium gypsum equilibrated the CO2. main reactions dissolution calcite that constitutes hydrotalcite por...

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