EGR Exploration Ltd V.EGR

Very Interesting News Release

[Diabolo]

Rare Earth Mineralized Carbonatite Intercepted in Carbo Diamond Drilling

September 13, 2011

Canadian International Minerals Inc (CIN-TSX.V) is pleased to announce that mineralized carbonatite and related alkaline rocks in significant intercepts have been intersected in the 2011 Phase I diamond drilling program on the Carbo Rare Earth Element (REE) property.

This first phase has focused on Targets, A, C, and D as outlined in our news release dated April 21, 2011. Target A is approximately 2000 meters south-east of Spectrum Resources 2008/09 drilling: select drill hole intersections from that program included 48.64 meters of 3.55% combined Rare Earth Elements (REEs), 144 meters of 2.2% combined REEs and 72 meters of 2.92% REEs. (Graf, Lane, Morrison, 2009). All intersection reported by Spectrum were collared in mineralization and assays were given in total elemental REEs which understates REE oxide content.

The area currently being drilled is defined by distinct airborne magnetic and radiometric anomalies, coincident rare earth element (REE) and pathfinder soil geochemical anomalies, and newly mapped carbonatite surface exposures. Diamond drill core from the first eight holes has been examined cursorily, and the first three holes have also been logged in detail. All of the holes have intersected intervals of mineralized carbonatite, associated alkaline rocks, and/or metasomatic alteration.

Drill Locations (Nad83 UTM Zone 10N), Hole Orientation and Depth

Target	Hole ID	Easting (m)	Northing (m)	Elev (m)	Azimuth	Inclination	EOH (m)
C	CA-11-010	561,336	6,041,339	1,344	232	-45	314
C	CA-11-011	561,464	6,041,122	1,376	232	-45	269
C	CA-11-012	561,464	6,041,122	1,376	52	-63	160
D	CA-11-013	562,112	6,040,317	1,443	250	-45	399
D	CA-11-014	561,978	6,040,523	1,439	223	-45	402
A	CA-11-015	560,049	6,041,485	1,415	N/A	-90	297
A	CA-11-016	560,049	6,041,485	1,415	230	-65	192
A	CA-11-017	560,049	6,041,485	1,415	50	-45	399
A	CA-11-018	559,940	6,041,178	1,481	50	-45	300
A	CA-11-019	559,940	6,041,178	1,481	50	-45	168

The following table is a summary ofalkaline rock intercepts (carbonatite, syenite and related dykes) observed to date.

Drillhole	From (m)	To (m)	Length (m)	Description
	161.63	164.17	2.54	Carbonatite
	171.80	191.24	19.44	Banded Carbonatite, Carbonatite, Syenite, Altered Sediments
CA-11-010	214.00	218.00	4.00	Carbonatite
	220.58	222.13	1.55	Carbonatite
	223.39	233.89	10.50	Banded Carbonatite, Syenite, Altered Sediments
	235.59	236.57	0.98	Banded Carbonatite
CA-11-011	125.00	143.67	18.67	Carbonatite, Banded Carbonatite, Syenite, Altered Carbonatite
	144.55	190.50	45.95	Banded Carbonatite, Altered Carbonatite, Carbonatite
	54.28	55.79	1.51	Carbonatite
	57.31	62.57	5.26	Syenite
	63.39	86.02	22.63	Altered Carbonatite, Banded Carbonatite, Syenite, Carbonatite
	94.80	104.31	9.51	Carbonatite, Banded Carbonatite, Green Breccia with Carbonatite Matrix
	130.19	234.51	104.32	Carbonatite, Green Breccia with Carbonatite Matrix, Grey Carbonatite, Grey Syenite, Altered Syenite
	245.35	245.82	0.47	Syenite
	249.25	251.68	2.43	Grey Syenite
	257.18	264.06	6.88	Alternating Carbonatite and Altered Sediments
CA-11-013	280.78	282.73	1.95	Carbonatite
	287.44	301.09	13.65	Syenite, Green Breccia with Carbonatite Matrix, Grey Syenite
	310.11	310.85	0.74	Syenite
	313.09	314.06	0.97	Carbonatite
	314.85	318.46	3.61	Carbonatite, Grey Syenite
	324.73	325.97	1.24	Altered Syenite
	330.72	335.93	5.21	Grey Syenite
	339.58	340.51	0.93	Grey Syenite
	342.20	357.55	15.35	Grey Syenite
	106.80	142.00	35.20	Carbonatite, Grey Syenite, Altered Syenite
	147.00	204.52	57.52	Grey Syenite, Carbonatite
CA-11-014	210.72	236.62	25.90	Carbonatite
	240.89	275.60	34.71	Grey Syenite, Carbonatite
	283.00	317.40	34.40	Grey Syenite, Carbonatite
	320.30	336.00	15.70	Syenite
CA-11-015	19.90	46.50	26.60	Syenite
	57.00	70.20	13.20	Syenite
CA-11-018	60.00	63.75	3.75	Syenite

Carbonatite and related alkaline units can be up to several tens of metres in thickness. These units are generally planar, and parallel to the host rock (phyllite) fabric, which is consistently subvertical, and trending approximately 140 degrees on surface. Occasionally the carbonatite occurs as crosscutting dykes or veins. The carbonatite is typically a combination of calcite, dolomite, and/or ankerite with a variety of accessory minerals including rare earth minerals. Many of the alkaline dykes are commonly sulphide-rich, and occasionally host sodalite. The host rocks around the carbonatite are commonly altered to varying degrees. The alteration may include bleaching, hornfelsing, riebeckite, and flooding of feldspar-feldspathoids.

Through visual examination, observation under short wave filtered and unfiltered ultra violet lights, and Niton XRF analysis, several mineral phases have been identified. Significantly elevated REE concentrations have been confirmed in select carbonatite samples when analyzed with a Niton XRF. Light rare earth elements (La, Ce, Pr and Nd), Ti, Nb, and Zn have been found to be elevated in some samples, implying the presence of associated mineral assemblages. This is consistent with what was observed in the 2010 drill core. Light pink and peach-coloured REE-bearing minerals have been observed in hand sample from outcrop and in drill core, and generally occur disseminated in the carbonatite or as cumulates. Other minerals identified visually are fluorite, ilmenite, sphalerite, pyrrhotite, pyrochlore, chalcopyrite, magnetite, and sodalite. Several samples have been chosen for further analysis by the University of British Columbia’s Mineralogical Research Group.

Core logging and property geological mapping at the Carbo is being led by Mallory Dalsin of Mackevoy Geosciences Ltd., who is in her second year on the project. Ms. Dalsin is completing a Master's thesis on the mineralogy, geochemistry and geochronology of the Wicheeda carbonatite complex at the University of British Columbia under the direction of Professor Lee Groat, a world renowned mineralogist. Ms. Dalsin is the recipient of a scholarship from Geoscience B.C. based on her study of the Carbo Project.

CIN has a multi-year drill permit for 30,000 meters, of which 5000 meters should be completed in the 2011 season ending late November. Core is being cut, logged, and stored at the company's expanded warehouse in Prince George, and samples are being sent to Activations Labs sample preparation facility in Stewart, B.C., with final analysis at their main laboratory in Ancaster, ON.

The Carbo property comprises 7 claims totalling 2,778.63 hectares in area, and is accessible by all weather gravel roads. It is approximately 80 km north east of Prince George, BC, a major provincial regional centre for mining, construction and logging industries. The project is approximately 40 km east of B.C. Hydro`s major electrical corridor and within 45 km of CN Rail's northern B.C. trunk line with connections to all of North America and the major ports of Prince Rupert and Vancouver.

The company is also awaiting final assays from the extensive surface stripping and trenching at its Dead Horse Creek and Prairie Lake projects. Currently all of the project geologists associated with that data collection and interpretation have been seconded to the Carbo Project to expedite the core logging, sampling and data handling processed. Final results will be released when available.

Mr. David Turner, M.Sc., P.Geo., an independent Qualified Person (as such term is defined by NI 43-101) is responsible for the review of technical information in this release.

Michael E. Schuss
President and Chief Executive Officer

“Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release."

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For further information please contact:

Dale Paruk
CoalHarborCommunications
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Email: [e-mail]

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