MORE HIGH-GRADE GOLD INTERCEPTS AT BUSHIANGALA

Description

• cours - matière potentielle : for the declaration of a maiden gold resource
• exposé

1 Unit 1, 245 Churchill Avenue Subiaco WA 6008 Australia PO Box 2025, Subiaco WA 6904 Phone: [phone] Fax: [phone] Email: ABN 31 009 235 956 ASX AND MEDIA ANNOUNCEMENT 21 December 2011 ELS 30/2012 MORE HIGH-GRADE GOLD INTERCEPTS AT BUSHIANGALA HIGHLIGHTS • Follow up drilling at Bushiangala continues to return very encouraging results: ASBSDD005 4.67m @ 4.92g/t Au from 77.95m ASBSDD006 6.34m @ 5.02g/t Au from 38.32m, and 16.00m @ 5.91g/t Au from 57.80m

• gold camp
• significant assays asrc0172 rc 687505 21629 220 -50 109.00 82.00 85.00 3.00 2.55 asrc0182 rc
• bushiangala
• bushiangala asbsdd0012 dd 687607 21293 220 -60 158.98 29.41 49.22 19.81 9.41 100.82 101.82 1.00 1205.00 asbsdd0022 dd 687445 21400 40 -50 155.82 103.93 104.93 1.00 5.15 153.00 154.00 1.00 1.49 asbsdd0032 dd
• rc
• results

Sujets

• Exposé
• Botswana Stock Exchange
• Edwards
• Kakamega
• Lake District

Informations

• Publié par: soom0
• Nombre de lectures: 17
• Langue: English
• Poids de l'ouvrage: 1 Mo

Extrait

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The University of the State of New York • THE STATE EDUCATION DEPARTMENT • Albany, New York 12234 • www.nysed.gov
Reference Tables for
Physical Setting/EARTH SCIENCE
Radioactive Decay Data Specific Heats of Common Materials
RADIOACTIVE DISINTEGRATION HALF-LIFE MATERIAL SPECIFIC HEAT
(years)ISOTOPE (Joules/gram • °C)
14 3 Liquid water 4.1814Carbon-14 N 5.7 × 10C
Solid water (ice) 2.11
40
40 Ar 9 Water vapor 2.00KPotassium-40 1.3 × 1040
Ca Dry air 1.01
9238 206 4.5 × 10Uranium-238 U Pb Basalt 0.84
Granite 0.79
1087 87 4.9 × 10Rubidium-87 Rb Sr Iron 0.45
Copper 0.38
Lead 0.13Equations
distance between foci
Eccentricity = Properties of Waterlength of major axis
change in field value Heat energy gained during melting . . . . . . . . . . 334 J/gGradient =
distance
Heat energy released during freezing . . . . . . . . 334 J/g
change in value Heat energy gained during vaporization . . . . . 2260 J/gRate of change =
time Heat energy released during condensation . . . 2260 J/g
mass
Density = Density at 3.98°C . . . . . . . . . . . . . . . . . . . . . . . . 1.0 g/mLvolume
Average Chemical Composition
of Earth’s Crust, Hydrosphere, and Troposphere
CRUST HYDROSPHERE TROPOSPHEREELEMENT
(symbol) Percent by mass Percent by volume Percent by volume Percent by volume
Oxygen (O) 46.10 94.04 33.0 21.0
Silicon (Si) 28.20 0.88
Aluminum (Al) 8.23 0.48
Iron (Fe) 5.63 0.49
Calcium (Ca) 4.15 1.18
Sodium (Na) 2.36 1.11
Magnesium (Mg) 2.33 0.33
Potassium (K) 2.09 1.42
Nitrogen (N) 78.0
Hydrogen (H) 66.0
Other 0.91 0.07 1.0 1.0
2010 EDITION Eurypterus remipes
This edition of the Earth Science Reference Tables should be used in the
classroom beginning in the 2009–2010 school year. The first examination for
which these tables will be used is the January 2010 Regents Examination in
New York State FossilPhysical Setting/Earth Science.L
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2 Physical Setting/Earth Science Reference Tables — 2010 Edition
Generalized Landscape Regions of New York State
Interior
Grenville Province
Lowlands
(Highlands)
Interior Lowlands
Adirondack
Mountains
Lake Ontario
Tug Hill
Plateau
Erie-Ontario Lowlands
(Plains)
Lake Erie
Allegheny Plateau
The Catskills
Key
Major geographic province boundary
Landscape region boundary
State boundary
International boundary
N
Miles
02100 3040 50
WE
020 40 60 80
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Manhattan Prong
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Physical Setting/Earth Science Reference Tables — 2010 Edition 3
Generalized Bedrock Geology of New York State
modified from
GEOLOGICAL SURVEY
NEW YORK STATE MUSEUM
1989
GEOLOGIC PERIODS AND ERAS IN NEW YORK
CRETACEOUS and PLEISTOCENE (Epoch) weakly consolidated to unconsolidated gravels, sands, and clays
LATE TRIASSIC and EARLY JURASSIC conglomerates, red sandstones, red shales, basalt, and diabase (Palisades sill)
Dominantly
PENNSYLVANIAN and MISSISSIPPIAN conglomerates, sandstones, and shales
sedimentary
DEVONIAN
limestones, shales, sandstones, and conglomerates
} origin
SILURIAN also contains salt, gypsum, and hematite.
SILURIAN
}
ORDOVICIAN
limestones, shales, sandstones, and dolostones
}
CAMBRIAN
CAMBRIAN and EARLY ORDOVICIAN sandstones and dolostones
moderately to intensely metamorphosed east of the Hudson River
Dominantly
CAMBRIAN and ORDOVICIAN (undifferentiated) quartzites, dolostones, marbles, and schists
metamorphosed
intensely metamorphosed; includes portions of the Taconic Sequence and Cortlandt Complex
rocks
TACONIC SEQUENCE sandstones, shales, and slates }
N
Miles
slightly to intensely metamorphosed rocks of CAMBRIAN through MIDDLE ORDOVICIAN ages
02100 3040 50
MIDDLE PROTEROZOIC gneisses, quartzites, and marbles
WE
Lines are generalized structure trends.
Intensely metamorphosed rocks
020 40 60 80OTEROZOIC anorthositic rocks } (regional metamorphism about 1,000 m.y.a.)
Kilometers S
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4 Physical Setting/Earth Science Reference Tables — 2010 Edition
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Surface Ocean Currents
20° 40° 60° 80° 100° 120° 140° 160° 180° 160° 140° 120° 100° 80° 60° 40° 20° 0° 20°
80°
Greenland
Arctic Ocean
Arctic Circle
(66.5° N)
60°
Asia
c
Europe
North
America
40°
North
North
Pacific
Atlantic
Florida C.
Ocean
Ocean Tropic of Cancer
(23.5° N)
India
20°
Africa
Africa u
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0° Equator
atorial
qu
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20°
Indian
Tropic of Capricorn
Ocean
(23.5° S)
Australia South South
Pacific Atlantic
Ocean Ocean
40°
60°
Antarctic Circle
(66.5° S)
Southern Ocean
Antarctica Antarctica
80°
20° 40° 60° 80° 100° 120° 140° 160° 180° 160° 140° 120° 100° 80° 60° 40° 20° 0° 20°
NOTE: Not all surface ocean currents are shown.
Key
Warm currents
Cool currents
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Physical Setting/Earth Science Reference Tables — 2010 Edition 5
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Tectonic Plates
Iceland
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