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Showing posts with label Geology. Show all posts
Showing posts with label Geology. Show all posts

Monday, 12 September 2016

Dip and Strike in Hindi with animation Geology Mining |




Here I have tried to clear basic concept of Dip and Strike terms with animation os seam, apparent dip, and true dip is also introduced in this video.
This is also important in Winning and Working

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Sunday, 21 June 2015

Copper Porphyry


Friday, 1 May 2015

Types of Wall Rock Alteration

Types of Wall Rock Alteration

Types of Wall Rock Alteration
Types of Wall Rock Alteration
1. Potassicalteration
ØPotassic (or K-silicate) alteration is characterized by the formation of new K-feldspar and/or biotite, usually together with minor sericite, chlorite, and quartz.
ØAccessory amounts of magnetite/hematite and anhydrite may occur associated with the potassicalteration assemblage.
ØIt typically represents the highest temperature form of alteration (500–600°C) associated with porphyry Cu-type deposits, forming in the core of the system and usually within the granite intrusion itself.
ØPyrite and minor chalcopyrite and molybdenite are the only ore minerals associated with this alteration.
ØNot all K-feldspar alteration is characterized by the presence of reddish colouration.

2. Phyllic(or sericitic) alteration
ØThis alteration style is the most common in a variety of hydrothermal ore deposits and forms over a wide temperature range by hydrolysis of feldspars to form sericite(fine-grained white mica), with minor associated quartz, chlorite, and pyrite.
ØPhyllicalteration is associated with porphyry Cu deposits, but also with mesothermalprecious metal ores and volcanogenic massive sulfide deposits in felsic rocks.

Types of Wall Rock Alteration

3.  Propylitic alteration
ØPropylitic alteration is probably the most widespread form of alteration.
ØIntermediate argillic alteration affects mainly plagioclase feldspars and is characterized by the formation of clay minerals kaolinite and the smectite group (mainly montmorillonite). It typically forms below about 250°C by H+ metasomatism and occurs on the fringes of porphyry systems.
ØAdvanced argillic alteration is characterized by kaolinite, pyrophyllite, or dickite (depending on the temperature) and alunite together with lesser quartz, topaz, and tourmaline. This type of alteration is characteristic of many epithermal precious metal deposits and a smaller number of mesothermal deposits such as Butte, Montana.

4. Silication

ØSilication is the conversion of a carbonate mineral or rock into a silicate mineral or rock. It is the main process which accompanies the prograde stage in the formation of polymetallicskarndeposits which develop when a fertile, acidic, magmatic fluid infiltrates a carbonate host rock.

 5. Silicification
ØSilicification should not be confused with silication and refers specifically to the formation of new quartz or amorphous silicaminerals in a rock during alteration.


Types of Wall Rock Alteration.

6. Carbonatization(Dolomitization)
ØIs the formation of carbonate minerals (calcite, dolomite, magnesite, siderite,etc.) during alteration of a rock. As dolomite in association with amphibolite, siderite in a banded iron-formation, or calcite in a granitic host.

7. Greisenization
ØA process of hydrothermal alteration in which feldspar and muscovite are converted to an aggregate of quartz, topaz, tourmaline, and lepidolite (i.e., greisen) by the action of water vapor containing fluorine. Ref

8. Tourmalinization
ØMedium to high temperature alteration. Associated with many tin and gold deposits. Quartz-sericite-tourmaline veins and alteration common.

Types of Wall Rock Alteration

9. Hematitization
ØAlteration that is associated with oxidizing fluidsoften results in the formation of minerals with a high Fe3+/Fe2+ ratio and, in particular, hematite with associated K-feldspar, sericite, chlorite, and epidote.

10. Fenitization
ØA fenite is a quartzofeldspathic rock that has been altered by alkali metasomatism at the contact of a carbonatiteintrusive complex. The process is called fenitization. Fenite is comprised mostly of alkalicfeldspar, with some aegirine, subordinate alkali-hornblende, and accessory sphene and apatite. Chemically, fenites are Na- and K-rich silicate rocks which develop at the contact between alkaline (carbonatite) igneous intrusions and their surrounding country rocks.

11. Chloritization
ØChlorite may result from alteration of mafic minerals or introduction of Fe and/or Mg. Very common surrounding plumbing of sea-floor massive sulfides.


12. Bleaching
ØNot characterized by any specific mineral assemblage, but rather a color change between altered and unaltered rock. Generally the result of oxidation of Fe.

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Alteration is a complex process of ion exchange whereby some constituents are removed, others are added and still others are merely redistributed. The physical effects of alteration include recrystallization, changes in permeability and changes in colour.

Carbonate rocks are characteristically recrystallized along the borders of a vein or near an igneous contact. Conversely argillization may reduce permeability of a rock, leaving the orebody enclosed within a relatively impermeable shell.

Colour changes include bleaching, darkening and production of aureoles (zones) of various colours. Pastel colours are especially prominent around certain ore deposits and may form conspicuous leads to the ore.

Pyrite is a standard alteration product around sulphide ore deposits (since iron is one of the most abundant metals in the earth's crust). Pyrite forms whenever sulfur is added to a host rock containing iron or ferro-magnesian minerals. Pyrite causes a striking colour change e.g. the pyritization of a red sandstone or shale will produce a bleached zone due to reduction of iron. Conversely, any pyritized rock is likely to be made conspicuous at the surface by oxidation of iron which will produce a red, brown-red or yellow weathered zone.
Unstable (not in equilibrium) rocks undergo physical and chemical changes (in order to attain equilibrium) in the presence of early ground preparing hydrothermal fluids of ore solutions.
The alteration may be very subtle (hydration of ferromagnesian minerals) to very intense (silicification of limestones). 
Indeed replacement ores are merely commercially valuable products of wallrock alteration. 
Wallrock alteration has been recognized a valuable tool in exploration, because the alteration haloes around many deposits, are widespread and easier to locate than the orebodies themselves. 
At various distances from a vein, the conditions of temperature and chemistry are usually different. As a result of this different types of alteration are likely to be produced simultaneously at various distances from the vein or fissure. For example, in the outer fringes of the alteration zone, the ferromagnesians may have been slightly hydrated while the interior zone was being silicified or sericitized, and the intermediate zone argillized. The product of this is a zoning of different alteration products arranged symmetrically around the central vein. In some deposits this zoning is conspicuous and may be an excellent guide to ore.
TYPES OF WALL-ROCK ALTERATION
Now coming to the exact question raised, the types are varied and manifold. About 10 types are being named as under though numerous permutations and combinations often tend to produce mixed variables. To name the types : Argillic(kaolin+montmorillonite+dickite+pyrophyllite), Potassic(potash feldspar+biotite), Phyllic(quartz+sericite+pyrite), Propylitic(chlorite+epidote+calcite), Silicification (quartz+chert), Dolomitization, Feldspathization, Greissenisation, Fenitizaztion and Bleaching.

Ref: Wallrock Alteration - S. Farooq, Dept of Geology Aligarh Muslim University, India

www.geol-amu.org/notes/m7-1-8.htm: Extracted from Google page (Internet Search).

Tuesday, 28 April 2015

Golden Sunlight Mine

Golden Sunlight Mine 
Golden Sunlight Mine



Location: Jefferson County, Montana, United States.
Products: Gold.
Owner: Barrick Gold Corporation.
Ore Type: Breccia pipe.
Reserves: Golden Sunlight produced 86,000 ounces of gold in 2014 at all in sustaining costs of $1,181 per ounce1. Proven and probable mineral reserves as at December 31, 2014, were 127,000 ounces of gold2.
In 2015, gold production is expected to be 90,000-105,000 ounces at all-in sustaining costs of $1,000-$1,025 per ounce.

Geological setting & Mineralization
The Golden Sunlight gold-silver deposit is hosted by a breccia pipe that cuts sedimentary rocks of the Middle Proterozoic Belt Supergroup and sills of a Late Cretaceous rhyolite porphyry (Porter and Ripley, 1985; Foster, 1991a, 1991b). At depth, rhyolite porphyry forms the matrix for fragments of the pipe. Creation of the pipe appears to be related to emplacement of an underlying hypabyssal stock related to the sills. Crosscutting the breccia pipe are hydrothermally altered lamprophyre dikes that postdate the gold-silver ore; locally, these dikes may have created areas of high-grade ore in the breccia pipe near their margins. The timing of emplacement of various igneous rocks and the hydrothermal alteration related to mineralization at the deposit.

Gold and silver in the region was concentrated along northeast-striking, high-angle faults and shear zones, some of which cut the breccia pipe and along which lamprophyre dikes have been emplaced (Porter and Ripley, 1985). These structures are thought to be part of a regional, northeast-striking zone of crustal weakness that has been intermittently active from the Proterozoic to the present (Foster and Chadwick, 1990; Foster 1991a). Because some hydrothermally altered and mineralized lamprophyre dikes are preferentially emplaced along structures that cross-cut the breccia pipe, their relationship to mineralization of the breccia pipe has been ambiguous. Certainly their emplacement is later than that of the pipe, and the simplest interpretation is that lamprophyre emplacement postdates mineralization. But, because the northeast-striking shear zones, veins, and dikes contain high-grade ore in places, a mineralizing process was obviously continuing during emplacement of the lamprophyre bodies.
 
Geologic cross section of the Golden Sunlight breccia pipe.
Geologic cross section of the Golden Sunlight breccia pipe.
Mine Life
Since its beginnings in 1982, Golden Sunlight Mine has continued to add resources to extend the life of the mine. Currently, the Montana DEQ is conducting the environmental review necessary to grant permission for mining additional resources referred to as the North Area Pit and South Area Layback, which would extend the mine life into 2016. Additional exploration is ongoing north of the Mineral Hill pit site with drilling activity in the Bonnie/Microwave area. 2013 will bring its own mix of success and challenge, so it is important that we remain intently focused on continuous improvement. As we work to deliver safe and profitable gold production, we cannot lose sight of our long-range goals—community partnership, environmental stewardship and most importantly, the safety and health of our people. I thank everyone again for the warm reception and look forward to getting to know you better in the coming months.

Safety and Health
We made great strides in improving our safety record, an achievement we celebrated in March, when we received Barrick’s Excellence Award for Best Safety Performance. As of first quarter 2013, GSM has gone five and a half years, and 2.7 million employee hours, without a lost-time incident, and over a year without a medical aid treatment incident. We still have more work to do in order to achieve our goal of zero incidents. As with most things, safety starts and ends with leadership. I expect all of our employees to be leaders when it comes to ensuring safety and continuing to send all GSM employees and contractors home safe and healthy every day.

Environment
Golden Sunlight Mine was the recipient of the prestigious Bureau of Land Management (BLM) 2012 Mineral Environmental Award for our third-party ore processing and reclamation initiatives. Golden Sunlight Mine initiated the program to assist small miners to mill outside “ores” and to assist with legacy mine materials containing reasonable concentrations of precious metals. In presenting the award, the BLM stated: “The Golden Sunlight Mine has turned liabilities into environmental and economic benefit—greatly enhancing the quality of the environment, saving taxpayer dollars, and creating local jobs.”

Sunday, 26 April 2015

Classification of Mineral Deposits

Depth of Occurrence

Exposedto surface

Mineral deposits like iron ore, bauxite, chromite, copper, limestone and magnesite are exposed to the surface and easy to explore. Although most of the significant exposed ore deposits, namely, Example Outside the Sterling Hill Mine are exposures of the weathered surface of the zinc ore body in the Passaic Pit.  Calamine (zinc silicate) was mined in this oxidized portion of the ore body. Canon City, USA.

Shallow Depth

Deposits like base metals, coal and gypsum are covered by altered oxidized capping or exist at shallow depth or under thick overburden of bedrock. The deposits are Cerro de Maimoncopper-gold deposit at Dominican Republic, Geochemical prospecting and ground geophysical survey will be helpful for discovery of deposits at shallow depth.

Deep-Seated Hidden Deposit

Deep-seated hidden deposits will be the future target of mineral exploration. The key exploration procedures suitable for discovery of an orebody at a depth range of 300-700 m require clear understanding of regional structure, applications of high penetrative geophysical methods and interpretation by simulation tools to identify, describe and delineate. Exploration for such deposits is expensive and associated with considerable economic risk. The high costs result from the necessity of expensive instrumentation and extensive drilling at depth. Ex. The hidden poly-metallic deposits discovered in the past are Neves Corvo copper-zinc-tin, Portugal, at 330-1000 m depth, and SindesarKhurd zinc lead-silver at 130 m depth, India.
Depth of Occurrence
Exposed to surface,Shallow depth, Deep-seated hidden deposit

Tuesday, 24 September 2013

Pumice stones | geology behind floating stone like in ramayan

It is mentioned in the epic Ramayana that Ram Setu was built by the son of Lord Vishwakarma when Lord Rama needed to cross the sea to reach Lanka. The epic mentions that whenever the name of Lord Rama was written over any stone, it started to float in the sea water.
As we are human and some questions occures in our mind for checking that presence of that thing in actual world.

YES IT IS TRUE, PUMICE STONE FLOATES OVER THE WATER. IT IS GEOLOGY DUDE....:-)
Any object floats in any liquid when the weight of the liquid, displaced by the fraction of the object immersed in the liquid, is equal to the entire weight of the object itself. Pumice called pumicite in its powdered or dust form, is a volcanic rock that consists of highly vesicular rough textured volcanic glass, which may or may not contain crystals. It is typically light colored. Pumice is created when super-heated, highly pressurized rock is violently ejected from a volcano . The unusual foamy configuration of pumice happens because of simultaneous rapid cooling and rapid depressurization. The depressurization creates bubbles by lowering the solubility of gases (including water and CO2 ) that are dissolved in the lava, causing the gases to rapidly exsolve (like the bubbles of CO2 that appear when a carbonated drink is opened). The simultaneous cooling and depressurization freezes the bubbles in the matrix.
Pumice has an average porosity of 90%, and initially floats on water. Pumice is widely used to make lightweight concrete or insulative low-density cinder blocks. When used as an additive for cement , a fine- grained version of pumice called pozzolan is mixed with lime to form a light-weight, smooth, plaster-like concrete.

Thursday, 8 August 2013

Download Book :: Dictionary of Geology and Mineralogy - McGraw-Hill

An amazing and very useful book for Mining Engineering students.

Dictionary of Geology Mineralogy, Second Edition
Publisher: McGraw-Hill | 420 pages | January 27, 2003 | ISBN 0071410449 | File type: PDF | 4 mb
Derived from the content of the respected McGraw-Hill Dictionary of Scientific and Technical Terms, Sixth Edition, each title provides thousands of definitions of words and phrases encountered in a specific discipline. All include:
* Pronunciation guide for every term
* Acronyms, cross-references, and abbreviations
* Appendices with conversion tables; listings of scientific, technical, and mathematical notation; tables of relevant data; and more
* A convenient, quick-find format


Download







  


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Sunday, 4 August 2013

Characteristics of the tailing dams

Characteristics of the tailing dams investigated.

(a) Drainage system-Germano tailings
(b) Drying bays of the Germano tailings dam (
c) Vertical drains – Drying bays of the Germano dam
(d) Vertical drain made of gabions
(e) Cava do Germano dam
(f) Drainage system of Fosfertil tailings dam.
Photo