Tuesday 23 February 2016
THE SOUNDS OF HELLFIRE IN EARTH ...THE RAT RACE TO THE WHITE HOUSE ...PRAISE THE WORD OF OUR FORD THE TIMES OF DOOM ARE AROUND THE CORNER ....THE NEW MADRID FAULT AND THE TECTONIC BLOWOUT OF YELLOW YOU ARE YELLOW OF 2016 THE APPS POST CALIPSO OF 2012 ARRIVE WITH A LITTLE TIME OUT TO TRUMPIC TIMES OF DOOM AND PUT IN TWO BLOWJOBS IN IT YOU'RE FIRED SAYS THE WALRUS TO THE CARPENTER
ARKANSAS WITH A BEACH BITCH
Monday 9 November 2015
AND FOR NOW THE INDIAN SUMMER GOES ON AND ON BUT AT NIGHT THE OLD PEOPLE FROM THE OLD WEST-COM CIVILIZATION SLOWLY BEGINS TO FREEZE - DA NATUREZA DA PROCURA DO SANTO GRAAL - AS MAIORES ANOMALIAS POSITIVAS SÃO NO MAR DO NORTE JUNTO A NARVIK UNS 9ºC E AS MENORES OU AS MAIORES NA NEGATIVA SÃO NA NAMÍBIA UNS - 9ºC PROCURA-SE UM AUMENTO DE UMA DÉCIMA DE GRAU POIS O OCEANO É DAS COUSAS MAIS ESTÁVEIS QUE EXISTE E 34ºC SÓ NO MAR VERMELHO OU 35ºC NO GOLFO PÉRSICO UNS SÍTIOS QUE COMPETEM COM SUCESSO COM O ALGARVE ATÉ CAIR UM AVIÃO NO RESTO DO MUNDO UM MAR TROPICAL ACIMA DOS 28ºC É COUSA MUY RARA E É A ZONA TROPICAL QUE TEM AS ÁGUAS MAIS QUENTES PARA OS TURISTAS E NÃO A EQUATORIAL....E VAI DAÍ OS RUSSOS PROCURAM ALTERNATIVAS AO MAR VERMELHO EM NOVEMBRO E AQUI NÃO AS ENCONTRAM DE CERTEZA E NO MAR DO NORTE A ÁGUA COMEÇA A GELAR E TENDO EM CONTA QUE A ÁGUA COM SAL GELA ABAIXO DOS 30,1ºF OU DOS - 1,9ºC PARA UMA SALINIDADE MÍNIMA DE 35%o 35 POR 1000.......O SLUSH JÁ COMEÇOU E ESPERA-SE UMA NOVA ANOMALIA DO VÓRTICE POLAR E UMA PROCURA DE PETRÓLEO E GÁS PARA AQUECER AS FRIAS GENTES DO NORTE E TAMBÉM VAI CHEGAR MAIS A SUL ....ECONOMICAMENTE O OUTONO-INVERNO DE 2015/2016 É CATASTRÓFICO PARA QUALQUER GOVERNO BASTA FAZER AS CON TÁSSE...À PROCURA DA BARATA TUTSI PROVAVELMENTE A MÁQUINA BIOLÓGICA MAIS PERFEITA QUE DEUS NA SUA INFINITA SABEDORIA CRIOU A BELEZA DESSE BICHO QUE SOBREVIVE A TODOS OS HOLOCAUSTOS MATA A BARATA TUTSI DIZEM OS HUMANOS E A BARATA TUTSI A TUDO SOBREVIVE.
10 VEZES MAIS RÁPIDA QUE UM SER
DITO HUMANO A BARATA TUTSI
VIVE NUM CONTÍNUO ESPAÇO
TEMPORAL DIFERENTE DO NOSSO
NÃO SE PREOCUPA COM COUSAS
COMO GOVERNOS, ALIANÇAS
OU OUTRAS B-LOUQUICES
A BARATA TUTSI SABE QUE
SOBREVIVERÁ A TUDO
A BARATA TUTSI É UM BICHO DE FÉ
E NA FÉ PROCRIA
ATÉ ENCHER O MUNDO
DITO HUMANO A BARATA TUTSI
VIVE NUM CONTÍNUO ESPAÇO
TEMPORAL DIFERENTE DO NOSSO
NÃO SE PREOCUPA COM COUSAS
COMO GOVERNOS, ALIANÇAS
OU OUTRAS B-LOUQUICES
A BARATA TUTSI SABE QUE
SOBREVIVERÁ A TUDO
A BARATA TUTSI É UM BICHO DE FÉ
E NA FÉ PROCRIA
ATÉ ENCHER O MUNDO
Tuesday 1 September 2015
NO VOTO QUE BOTO NA PREGA DA NEGRA URNA DIURNA PONHO MUITO DISCRETO O PRETO NO BRANCO NUM TRANCO PRA QUEBRAR SE CALHAR O ENCANTO DO QUEBRANTO ....DO HIPNOVOTO TAMBÉM JESUS É DEVOTO E TODO O CARRASCO USA CAPUZ NO HIPNOVETO QUE É MAIS DISCRETO JÁ O HIPNOPUTO É ASTUTO E NO LONGE OU NO PERTO ESTÁ SEMPRE CERTO E NUNCA FICA NUM APERTO..mexiânica cromada e zinkada à pedrada de cavalo na veia
EM VERDADE VOS DIGO
QUE NESTA SECA FRÁGUA
NÃO VEJO SOMBRA D'ÁGUA
NEM DE MÁGOA COSTA AMIGO
E SÓ NA FÉ CLARA E VERDADEIRA
NO VOTO DEVOTO E PERDIDO
NO VOTO COMPRADO OU PEDIDO
NESTA DEMO AFINAL A DERRADEIRA
NO VOTO SE DESARMA A ALMA CALMA
O VOTO EM TODO CÉSAR METE PALMA
OU LOUROS
OU OUTROS TEMPEROS
NO VOTO DADO EM VÃO
NASCE PIEDADE E ATÉ PERDÃO
NO CAMINHO LONGE OU PERTO
FEITO NA CRUZ EM QU'ACERTO
NUNCA SERÁ CAMINHO CERTO
QUE NESTA SECA FRÁGUA
NÃO VEJO SOMBRA D'ÁGUA
NEM DE MÁGOA COSTA AMIGO
E SÓ NA FÉ CLARA E VERDADEIRA
NO VOTO DEVOTO E PERDIDO
NO VOTO COMPRADO OU PEDIDO
NESTA DEMO AFINAL A DERRADEIRA
NO VOTO SE DESARMA A ALMA CALMA
O VOTO EM TODO CÉSAR METE PALMA
OU LOUROS
OU OUTROS TEMPEROS
NO VOTO DADO EM VÃO
NASCE PIEDADE E ATÉ PERDÃO
NO CAMINHO LONGE OU PERTO
FEITO NA CRUZ EM QU'ACERTO
NUNCA SERÁ CAMINHO CERTO
Monday 16 March 2015
E SOMBRIOS GOVERNOS EM LÚGUBRES CANTOS....LUGUBREMENTE SE ASSENTAM EM ACENTOS...EM DUROS FERROS DE HIRTOS ENCANTOS....EM PENETRANTES URROS AOS CENTOS....COM VÍRGULAS ASSOMANDO DOS HIRSUTOS PEITOS....SOLTAM ENREDOS DE VELHOS DESPEITOS...E DE FORTUNAS EM BANCOS DESFEITOS ...POR SANTOS ESPÍRITOS MAIS QUE PERFEITOS,,,E ASSIS LANÇAM PALAVRAS COMO CONFEITOS...ENQUANTO OS FACTOS SOFREM CUIDADOS ...CUIDANDO QUE SÃO COMO OS FADOS...QUE EM FALSAS PALAVRAS NOS LIBERTAM....QUANDO AS VERDADES EM NÓS NOS APERTAM ...
E
EM VERDADEIRAS REVOADAS....
OS FALSOS VEROS MESSIAS.....
LANÇAM VERDADES MUY USADAS ...
QUE ATÉ À FALSIDADE DÃO AZIAS .....
E ESTAS VERDADES ACEITAI ....
E NÃO CUIDEIS SE EM VERDADE VEM OU VAI.....
OU SE NOUTRAS PORRAS SE ESVAI ....QUANDO A FALSA IDADE SOBE OU CAI...
OU SOBRE VÓS EM NÓS CAI....
OS FALSOS VEROS MESSIAS.....
LANÇAM VERDADES MUY USADAS ...
QUE ATÉ À FALSIDADE DÃO AZIAS .....
E ESTAS VERDADES ACEITAI ....
E NÃO CUIDEIS SE EM VERDADE VEM OU VAI.....
OU SE NOUTRAS PORRAS SE ESVAI ....QUANDO A FALSA IDADE SOBE OU CAI...
OU SOBRE VÓS EM NÓS CAI....
Saturday 28 February 2015
Monday 3 November 2014
DESDE 1 DE NOVEMBRO DE 1755 ....259 ANOS DE FALHANÇOS NAS PREVISÕES DO APOCALIPSE .....GLOBAL GEOLOGIC AND HYDROLOGICAL CHANGES
Beware the power of ....
Mental note's:
never park vehicle at DUNMOVIN, CA or it may not be dunmovin. ;)
OverwhelmingSilence Holy shit.
or in simplified views
Oh shit.
THE GLOBAL WARMING Effects
MORE WTF AGW EFFECTS
Mental note's:
never park vehicle at DUNMOVIN, CA or it may not be dunmovin. ;)
OverwhelmingSilence Holy shit.
or in simplified views
Oh shit.
THE GLOBAL WARMING Effects
MORE WTF AGW EFFECTS
Friday 20 June 2014
SHEETED DYKE SWARMS - LAYERED GABBROIC ROCKS - FAULT ZONES - STOCKWORKS THAT DON'T WORK AND MASSIVE SULPHIDE DEPOSITS
The most common sulfide mineral in VMS deposits is pyrite, which is often associated with other sulfides such as pyrrhotite, chalcopyrite, sphalerite, and galena (Galley and others, 2007). Other possible nonsulfide minerals associated in VMS deposits include magnetite, hematite, and cassiterite; barite can be present as a gangue mineral. All these minerals have relatively high values of specific gravity (4.0–7.5 g/cm3; table 7–2), which is in strong contrast to the significantly lower densities measured in their sedimentary or volcanic host rocks. Thomas (2003) measured densities of 2.70–2.84 g/ cm3 for the host rock at the Bathurst mining camp.
Electrical Signature
Electrical methods are highly effective in identifying VMS targets because they respond to the electrical conductivity of the rocks and minerals, which can vary by 20 orders of magnitude (Grant and West, 1965). Electrical methods are unique in being able to detect such a large range of magnitudes; no other physical property has such a wide range. Because of this large potential range in values, a variety of electrical techniques have been developed that capitalize on these differences, such as measurement of conductivity, resistivity (the inverse of conductivity), induced polarization, electromagnetism, and gamma ray spectra (table 7–1). Electrical methods are currently the most used technique in surveying for VMS deposits; a variety of survey types (for example, MegaTEM, Titan24, and borehole techniques) are pushing the limits of detectable depth ranges.
Volcanogenic massive sulfide deposits have high conductivities (fig. 7–2B) exceeding 500 mS/m (millisiemens per meter) and are similar in magnitude to graphite and saltwater (Ford and others, 2007). Compared to igneous and metamorphic rocks with typical conductivities of <1 1="" 500="" a="" also="" and="" anoxic="" are="" as="" associated="" be="" between="" body.="" body="" br="" by="" can="" complicating="" conductive="" conductivities="" conductivity="" contain="" content="" contrast="" could="" definitive="" deposits.="" deposits="" difficult="" distinguish="" distinguishable="" economic="" effectively="" electromagnetic="" exploration="" factor="" from="" fully="" graphite="" highly="" horizons="" host="" however="" in="" increase="" introduced="" its="" m="" mask="" massive="" may="" ms="" noneconomic="" not="" of="" or="" ore="" other="" overlying="" physical="" potentially="" property.="" pyrite-rich="" pyrrhotite-rich="" reducing="" rock="" rocks="" sedimentary="" sediments.="" signal="" significant="" so="" some="" substantially="" such="" sulfide="" techniques="" that="" the="" themselves.="" thus="" to="" tools="" types="" typically="" unit="" useful="" vms="" water-rich="" water="" with="">Electrical resistivity surveys are useful in calculating the apparent resistivity of the subsurface at different depths resulting in the generation of cross sections of true resistivity (Ford and others, 2007). These can be used to produce three-dimensional geometries of ore bodies at depth. Resistivity surveys also are used to estimate the thickness of overburden, which
7. Geophysical Characteristics of Volcanogenic Massive Sulfide Deposits
By Lisa A. Morgan
118 7. Geophysical Characteristics of Volcanogenic Massive Sulfide Deposits
Figure 7–1. Schematic diagram of the modern Trans-Atlantic Geothermal (TAG) sulfide deposit on the Mid-Atlantic Ridge, depicting a cross section of a volcanogenic massive sulfide deposit with concordant semi-massive to massive sulfide lens underlain by a discordant stockwork vein system and associated alteration halo. From Hannington and others (1998) and Galley and others (2007). Modified from Hannington and others (2005).
then can be used to improve interpretation of ground gravity surveys (Ford and others, 2007). Conductivity, the inverse of resistivity, also can be used to map overburden.
Induced polarization (IP) surveys measure the chargeability of the ground and the time variance in the response of the electromagnetic field, which is related to ability of the material to retain electrical charges. Induced polarization surveys are very effective in detecting disseminated sulfide bodies. Typically, these sulfides occur in the altered halo surrounding the massive sulfide ore body and may be associated with clays, which also produce significant IP responses (Ford and others, 2007).
The techniques associated with electromagnetic (EM) surveys, collected both on ground and in air, are the most common electrical methods employed in mineral exploration. Electromagnetic techniques can directly detect conductive features such as base metal deposits where significant contrasts in conductivity values occur between the ore bodies and their resistive host rocks (Thomas and others, 2000). Values for the conductivity of soils, rocks, and ore bodies, measured in milliSiemans per meter, span several orders of magnitude ranging from 3.57×109 mS/m for graphite to 5×108 mS/m for pyrrhotite to 0.01 mS/m for gravel and sand (Thomas and others, 2000). Both airborne and ground electromagnetic techniques are effective in detecting1>
Electrical Signature
Electrical methods are highly effective in identifying VMS targets because they respond to the electrical conductivity of the rocks and minerals, which can vary by 20 orders of magnitude (Grant and West, 1965). Electrical methods are unique in being able to detect such a large range of magnitudes; no other physical property has such a wide range. Because of this large potential range in values, a variety of electrical techniques have been developed that capitalize on these differences, such as measurement of conductivity, resistivity (the inverse of conductivity), induced polarization, electromagnetism, and gamma ray spectra (table 7–1). Electrical methods are currently the most used technique in surveying for VMS deposits; a variety of survey types (for example, MegaTEM, Titan24, and borehole techniques) are pushing the limits of detectable depth ranges.
Volcanogenic massive sulfide deposits have high conductivities (fig. 7–2B) exceeding 500 mS/m (millisiemens per meter) and are similar in magnitude to graphite and saltwater (Ford and others, 2007). Compared to igneous and metamorphic rocks with typical conductivities of <1 1="" 500="" a="" also="" and="" anoxic="" are="" as="" associated="" be="" between="" body.="" body="" br="" by="" can="" complicating="" conductive="" conductivities="" conductivity="" contain="" content="" contrast="" could="" definitive="" deposits.="" deposits="" difficult="" distinguish="" distinguishable="" economic="" effectively="" electromagnetic="" exploration="" factor="" from="" fully="" graphite="" highly="" horizons="" host="" however="" in="" increase="" introduced="" its="" m="" mask="" massive="" may="" ms="" noneconomic="" not="" of="" or="" ore="" other="" overlying="" physical="" potentially="" property.="" pyrite-rich="" pyrrhotite-rich="" reducing="" rock="" rocks="" sedimentary="" sediments.="" signal="" significant="" so="" some="" substantially="" such="" sulfide="" techniques="" that="" the="" themselves.="" thus="" to="" tools="" types="" typically="" unit="" useful="" vms="" water-rich="" water="" with="">Electrical resistivity surveys are useful in calculating the apparent resistivity of the subsurface at different depths resulting in the generation of cross sections of true resistivity (Ford and others, 2007). These can be used to produce three-dimensional geometries of ore bodies at depth. Resistivity surveys also are used to estimate the thickness of overburden, which
7. Geophysical Characteristics of Volcanogenic Massive Sulfide Deposits
By Lisa A. Morgan
118 7. Geophysical Characteristics of Volcanogenic Massive Sulfide Deposits
Figure 7–1. Schematic diagram of the modern Trans-Atlantic Geothermal (TAG) sulfide deposit on the Mid-Atlantic Ridge, depicting a cross section of a volcanogenic massive sulfide deposit with concordant semi-massive to massive sulfide lens underlain by a discordant stockwork vein system and associated alteration halo. From Hannington and others (1998) and Galley and others (2007). Modified from Hannington and others (2005).
then can be used to improve interpretation of ground gravity surveys (Ford and others, 2007). Conductivity, the inverse of resistivity, also can be used to map overburden.
Induced polarization (IP) surveys measure the chargeability of the ground and the time variance in the response of the electromagnetic field, which is related to ability of the material to retain electrical charges. Induced polarization surveys are very effective in detecting disseminated sulfide bodies. Typically, these sulfides occur in the altered halo surrounding the massive sulfide ore body and may be associated with clays, which also produce significant IP responses (Ford and others, 2007).
The techniques associated with electromagnetic (EM) surveys, collected both on ground and in air, are the most common electrical methods employed in mineral exploration. Electromagnetic techniques can directly detect conductive features such as base metal deposits where significant contrasts in conductivity values occur between the ore bodies and their resistive host rocks (Thomas and others, 2000). Values for the conductivity of soils, rocks, and ore bodies, measured in milliSiemans per meter, span several orders of magnitude ranging from 3.57×109 mS/m for graphite to 5×108 mS/m for pyrrhotite to 0.01 mS/m for gravel and sand (Thomas and others, 2000). Both airborne and ground electromagnetic techniques are effective in detecting1>
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