Join today and have your say! It’s FREE!

Become a member today, It's free!

We will not release or resell your information to third parties without your permission.
Please Try Again
{{ error }}
By providing my email, I consent to receiving investment related electronic messages from Stockhouse.

or

Sign In

Please Try Again
{{ error }}
Password Hint : {{passwordHint}}
Forgot Password?

or

Please Try Again {{ error }}

Send my password

SUCCESS
An email was sent with password retrieval instructions. Please go to the link in the email message to retrieve your password.

Become a member today, It's free!

We will not release or resell your information to third parties without your permission.
Quote  |  Bullboard  |  News  |  Opinion  |  Profile  |  Peers  |  Filings  |  Financials  |  Options  |  Price History  |  Ratios  |  Ownership  |  Insiders  |  Valuation

Queen's Road Capital Investment Ltd T.QRC

Alternate Symbol(s):  BRSGF

Queen's Road Capital Investment Ltd is a financier to the global resource sector. The Company is a resource-focused investment company, making investments in privately held and publicly traded resource companies. The Company acquires and hold securities for both long-term capital appreciation and short-term gains, with a focus on convertible debt securities and resource projects in development or production located in safe jurisdictions.


TSX:QRC - Post by User

Post by GeneralKesefon Nov 20, 2013 5:00pm
263 Views
Post# 21924759

JUST BEFORE YOU CLOSE YOUR COMPUTOR

JUST BEFORE YOU CLOSE YOUR COMPUTORREAD THE OPPORTUNITY

SEE YOY ALL AT 5 AM


Potential for carbonate‐hosted mineralisation
 
Barisan appears comparable in some ways to the highlands of PNG, in that there appears to be the potential for a limestone ‘cap’ or ‘lid’ on the district. In New Guinea, Porgera, Ok Tedi and Grasberg all occur at or near the base of the New Guinea limestone or equivalent unit (Gow and Walshe, 2005), and this type of stratigraphic architecture is believed to have been favorable for the confinement of vola tiles and development
of high‐grade mineralization.
 
Given the geological architecture of the Barisan district, and the presence of late‐stage, apparently quite intensely acidic fluids (particularly at Upper Tengkereng – where drilling is now), there may be an opportunity for targeting an unusual style of hybrid mineral deposit within the limestone ‘cap’ to the district. The Colquijirca and Cerro de Pasco deposits in Peru are examples of carbonate‐hosted high sulfidation deposits. In these examples, acidic magmatic‐hydrothermal fluids have interacted with highly reactive carbonate wallrocks (e.g., Fig. 6), which have provided an excellent chemical trap, resulting in up to 8 km of along‐strike sulfide mineralization at Colquijirca, zoned from a core of Cu‐Au thro gh Pb‐Zn to distal Ag‐ Bi. Barisan appears to be overlain by limestone, and it is possible that the acidic fluids that produced the clay alteration at Upper Tengkereng and/or Upper Ise migrated upwards into this ‘infinite ’ reservoir of acid‐ neutralising wall rock. If this happened, then any metals carried by those acidic fluids should have been precipitated during acid neutralization, producing carbonate‐hosted ores that could contain several percent Cu and base metal sulfides intergrown with alunite and clay minerals. Geochemical sampling at the base of the limestone and mapping of fault corridors that connect the porphyries with the limestone es may provide targets for this style of mineralizatio

reading and learning about the opportunity is essential before making decisions, thats why i do my research before commiting heavy dollars

you too must do your own research

general Kesef

Bullboard Posts