Mapa Geológico do Sistema de Nappes Carrancas na região de ... · Legenda Convenções...
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Legenda Convenções Cartográficas Drenagens Curvas de Nível / Escala Numérica 1 : 50.000 IGc- USP- 2012 Dados coletados com apoio da turma de Mapeamento Geológico 2008-2010 orientada pelos professores Mario Campos da Costa Neto, Renato de Moraes e Marcos Egydio da Silva. Integração Gelógica realizada por Leandro Coutinho Estruturas e elementos estruturais S " L4- Crenulação e intersecção S " L3- Crenulação e intersecção S L2- Estiramento, intersecção e mullions h S4- Clivagem de crenulação zonal ou discreta h S3- Clivagem de crenulação zonal ou discreta Localmente xistosidade contínua transpondo S2 h S2- Clivagem espada e/ou xistosidade S2 (Foliação principal) Contato Normal S0//S2 F Antiforma Aberta D3 ou D4 M Sinforma Aberta D3 ou D4 P Sinforma Fechada D2 ou D3 I Antiforma Fechada D3 ou D4 ((( Contato de Cavalgamento D2 Zonas de Cisalhamento D3 Unidades Litoestratigráficas Neoproterozóico Grupo Carrancas Alóctone Muscovita quartzitos e muscovita-quartzo xistos com intercalações subordinadas de muscovita xisto, ambos com muscovita esverdeada. Fm. Chapada das Perdizes Muscovita quartzitos e muscovita-quartzo xistos com intercalações subordinadas de muscovita xisto, ambos com muscovita esverdeada. Fm. São Tomé das Letras Muscovita xistos grafitosos +/- porfiroblásticos (Cld, Grt, Ky, St) que gradam lateralmente para clorita-muscovita xistos. Fácie de intercalação métrica entre muscovita quartzitos e xistos grafitosos Muscovita quartzitos com níveis milimétricos de xisto grafitoso. Fm. Campestre Unidade Alóctone Granada-clorita-biotita-muscovita-quartzo xisto Embasamento e infraestrutura Arqueano e Paleoproterozóico Biotita gnaisse fino bandado com intercalaçôes de rochas meta-ultramáficas, anfibolitos e calciossilicáticas Meta-ultramáficas Granitóides tectonizados Ortognaisses migmatíticos com intercalações de rochas anfibolíticas, meta-ultramáficas e sedimentos do tipo greenstone belts Quartzitos e muscovita xistos associados a rochas meta-ultramáficas. Faixas do tipo "greenstone belts". Btx Cxg Ci Cq CPq STq Apu Apgb Ap1 Ap2 Ap3 ( ( ( ( ( ( ( ( (( (( (( ( ( ( (( ( (( ( ( (( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( (( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( (( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( ( 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S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " S " 32 44 90 15 85 80 84 75 38 85 42 55 90 75 77 82 90 40 82 70 80 21 23 43 38 56 70 58 60 75 80 70 85 78 87 30 86 20 68 28 60 77 66 80 75 85 1 5 60 24 40 30 75 75 31 50 47 62 60 75 25 53 53 82 70 60 70 35 86 86 75 38 80 85 55 60 32 57 70 48 35 30 73 80 74 45 85 85 65 32 65 70 25 30 15 60 55 52 45 12 25 30 30 40 50 85 88 75 68 40 79 58 35 60 45 58 83 70 60 65 47 86 40 50 65 80 55 53 6 5 5 9 7 8 5 5 5 5 5 2 2 8 6 5 6 4 3 5 5 5 3 4 5 7 8 4 5 8 8 2 4 5 0 5 7 8 4 5 4 5 6 5 6 5 8 6 1 3 5 30 65 50 45 42 45 20 45 50 55 55 50 25 60 65 52 40 35 35 45 25 20 15 20 23 12 20 22 15 20 20 25 25 21 32 10 30 25 15 16 25 25 17 12 25 16 30 21 50 15 20 25 20 25 37 46 27 16 29 20 35 35 29 14 20 22 32 30 45 16 69 22 10 37 46 70 20 16 34 29 16 11 25 29 11 30 60 28 64 15 35 45 80 79 50 82 30 51 20 10 90 55 76 65 50 42 60 47 25 70 10 30 70 66 80 55 60 10 55 80 15 54 37 45 58 55 56 50 15 76 66 60 45 68 46 50 60 42 42 80 42 70 36 57 60 62 60 34 45 57 43 60 65 47 45 63 37 35 67 50 75 55 81 70 56 80 60 45 49 36 50 60 46 62 55 45 44 81 50 30 85 64 58 81 28 54 74 62 86 72 79 60 19 17 61 83 55 64 45 65 28 20 15 19 10 25 51 30 20 63 60 29 15 20 12 10 10 15 68 24 42 22 15 42 32 12 27 52 13 46 15 60 20 31 10 15 30 20 16 18 26 15 18 20 22 15 12 35 30 20 15 24 23 10 15 16 12 28 17 10 44 15 30 12 10 34 11 20 37 20 20 12 17 25 30 27 10 20 21 15 14 15 30 10 35 28 46 19 16 60 25 20 35 27 35 34 20 12 20 20 25 20 15 53 21 55 17 25 15 15 20 20 25 35 30 33 55 30 45 25 22 25 27 20 27 19 47 56 22 20 20 18 10 21 37 15 38 24 15 40 37 23 20 15 45 49 25 45 30 26 26 17 16 35 12 14 18 16 23 19 24 20 19 16 30 36 20 45 35 24 42 16 15 18 18 20 35 30 39 30 26 25 40 18 12 35 36 15 35 37 30 17 87 35 35 15 35 55 60 63 50 13 50 61 65 56 15 10 50 10 25 46 69 24 45 10 35 65 40 14 20 20 45 45 60 68 63 60 55 36 40 48 30 35 35 42 50 32 25 17 28 12 35 45 25 30 36 30 20 35 35 30 27 15 12 10 15 10 10 10 15 20 15 15 42 30 10 30 35 10 14 28 15 30 28 24 15 15 18 28 18 14 13 24 35 20 25 35 35 20 15 10 33 43 16 26 78 42 10 42 35 15 15 47 20 28 66 62 30 70 45 45 12 30 25 35 32 50 30 40 30 30 40 49 30 75 24 33 25 50 35 73 50 35 67 72 43 46 67 55 56 82 35 75 30 46 20 65 84 69 65 50 60 48 20 25 45 50 56 50 45 60 48 35 35 56 43 63 35 60 95 40 55 65 35 47 62 80 41 50 60 40 30 60 60 60 59 45 50 20 47 43 25 70 50 65 78 60 45 30 45 50 30 65 88 50 25 55 50 45 55 35 60 62 25 66 87 40 50 70 70 30 65 50 47 50 65 59 45 40 70 40 85 62 60 65 60 66 50 60 40 45 510000 ,000000 510000 ,000000 512000 ,000000 512000 ,000000 514000 ,000000 514000 ,000000 516000 ,000000 516000 ,000000 518000 ,000000 518000 ,000000 520000 ,000000 520000 ,000000 522000 ,000000 522000 ,000000 524000 ,000000 524000 ,000000 526000 ,000000 526000 ,000000 528000 ,000000 528000 ,000000 530000 ,000000 530000 ,000000 532000 ,000000 532000 ,000000 534000 ,000000 534000 ,000000 536000 ,000000 536000 ,000000 538000 ,000000 538000 ,000000 540000 ,000000 540000 ,000000 542000 ,000000 542000 ,000000 544000 ,000000 544000 ,000000 546000 ,000000 546000 ,000000 548000 ,000000 548000 ,000000 7610000 ,000000 7610000 ,000000 7612000 ,000000 7612000 ,000000 7614000 ,000000 7614000 ,000000 7616000 ,000000 7616000 ,000000 7618000 ,000000 7618000 ,000000 7620000 ,000000 7620000 ,000000 7622000 ,000000 7622000 ,000000 7624000 ,000000 7624000 ,000000 7626000 ,000000 7626000 ,000000 7628000 ,000000 7628000 ,000000 7630000 ,000000 7630000 ,000000 7632000 ,000000 7632000 ,000000 7634000 ,000000 7634000 ,000000 7636000 ,000000 7636000 ,000000 7638000 ,000000 7638000 ,000000 7640000 ,000000 7640000 ,000000 7642000 ,000000 7642000 ,000000 Mapa Geológico do Sistema de Nappes Carrancas na região de Itutinga, Itumirim, Carrancas e Minduri Metros 0 2.500 5.000 7.500 10.000 D4 D4 D3//D2 D3 D3 D3 D3//D2 D3//D2 D3 D3 D3 D3 D4 D2//D3 D2//D3 Tarde D3 D2//D3 D2//D3 D3 Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Btx Apgb Apgb Apgb Apgb Apgp Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Apu Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ag1 Ap3 Ap3 Ap3 Ap3 Ap3 Ap3 Ap3 Ap3 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 Ap2 CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq CPq STq STq STq STq STq STq STq STq STq Ap2 STq STq STq STq STq STq STq STq STq STq STq STq STq STq CPq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cq Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Cxg Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci Ci A A' B' B C' C D' D E' E F' F G G' H H' I' I
Transcript of Mapa Geológico do Sistema de Nappes Carrancas na região de ... · Legenda Convenções...
Legenda
Convenções CartográficasDrenagens Curvas de Nível
/Escala Numérica
1 : 50.000
IGc- USP- 2012Dados coletados com apoio da turma de Mapeamento Geológico 2008-2010
orientada pelos professores Mario Campos da Costa Neto, Renato de Moraes e Marcos Egydio da Silva.Integração Gelógica realizada por Leandro Coutinho
Estruturas e elementos estruturais
S" L4- Crenulação e intersecção
S" L3- Crenulação e intersecção
S L2- Estiramento, intersecção e mullions
h S4- Clivagem de crenulação zonal ou discreta
h S3- Clivagem de crenulação zonal ou discreta Localmente xistosidade contínua transpondo S2
h S2- Clivagem espada e/ou xistosidade S2 (Foliação principal)
Contato Normal S0//S2
FAntiforma Aberta D3 ou D4
M Sinforma Aberta D3 ou D4
P Sinforma Fechada D2 ou D3
I
Antiforma Fechada D3 ou D4
(( (( (( Contato de Cavalgamento D2
Zonas de Cisalhamento D3
Unidades Litoestratigráficas
Neop
rotero
zóico
Grupo Carrancas Alóctone
Muscovita quartzitos e muscovita-quartzo xistos com intercalações subordinadas de muscovita xisto, ambos com muscovita esverdeada.
Fm. C
hapa
dada
s Perd
izes
Muscovita quartzitos e muscovita-quartzo xistos com intercalações subordinadas de muscovita xisto, ambos com muscovita esverdeada.
Fm. S
ão To
méda
s Letr
as
Muscovita xistos grafitosos +/- porfiroblásticos (Cld, Grt, Ky, St) que gradam lateralmente para clorita-muscovita xistos.
Fácie de intercalação métrica entre muscovita quartzitos e xistos grafitosos
Muscovita quartzitos com níveis milimétricos de xisto grafitoso.Fm. C
ampe
stre
Unidade AlóctoneGranada-clorita-biotita-muscovita-quartzo xisto
Embasamento e infraestrutura
Arqu
eano
e
Paleo
proter
ozóic
o Biotita gnaisse fino bandado com intercalaçôes de rochas meta-ultramáficas, anfibolitos e calciossilicáticas Meta-ultramáficas
Granitóides tectonizados
Ortognaisses migmatíticos com intercalações de rochas anfibolíticas, meta-ultramáficas e sedimentos do tipo greenstone belts
Quartzitos e muscovita xistos associados a rochas meta-ultramáficas. Faixas do tipo "greenstone belts".
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STq
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ApgbAp1
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512000,000000
512000,000000
514000,000000
514000,000000
516000,000000
516000,000000
518000,000000
518000,000000
520000,000000
520000,000000
522000,000000
522000,000000
524000,000000
524000,000000
526000,000000
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528000,000000
528000,000000
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532000,000000
532000,000000
534000,000000
534000,000000
536000,000000
536000,000000
538000,000000
538000,000000
540000,000000
540000,000000
542000,000000
542000,000000
544000,000000
544000,000000
546000,000000
546000,000000
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000,00
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000,00
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0000
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Mapa Geológico do Sistema de Nappes Carrancas na região de Itutinga, Itumirim, Carrancas e Minduri
Metros0 2.500 5.000 7.500 10.000
D4
D4
D3//D2
D3
D3
D3
D3//D2
D3//D2
D3
D3
D3
D3
D4
D2//D3
D2//D3Tarde D3
D2//D3
D2//D3
D3
Btx
Btx
Btx
Btx
Btx Btx
Btx
Btx
Btx
Btx
Btx
Btx
Btx
Btx
Btx
Btx
Apgb
Apgb
Apgb
Apgb
Apgp
Apu
Apu
ApuApu
Apu
Apu
Apu
Apu
Apu
Apu
Apu
Apu
Apu
Apu
Apu
Apu Apu
Apu
Apu
ApuApu
Apu
Apu
Apu
Ag1
Ag1
Ag1
Ag1 Ag1
Ag1 Ag1
Ag1
Ag1 Ag1
Ag1
Ag1
Ag1
Ag1
Ag1
Ap3
Ap3 Ap3 Ap3
Ap3
Ap3
Ap3Ap3
Ap2Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
Ap2
CPqCPq
CPq
CPq
CPq
CPq
CPq
CPqCPq
CPq
CPq
CPq
CPq
CPq
CPq
CPq
CPq
CPq
CPq
CPqCPqCPq
CPqCPq
CPq
CPq
CPq
CPq
CPq
CPqCPqCPq
STq
STq
STq
STq
STq
STq
STq
STq
STq
Ap2
STq
STq
STq
STq
STqSTq
STq
STq
STq
STq
STq
STqSTq
STq
CPq
Cq
Cq
Cq
Cq
CqCq
Cq
CqCq
Cq
Cq
Cq
Cq
Cq
Cq
Cq
Cq
Cq
Cq
CqCq
CqCq
Cq
Cq
CqCq
CqCq
CqCqCq
Cq
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Cxg
Cxg
Cxg
Cxg
Cxg
Cxg
Cxg
Cxg
Cxg
Cxg
Cxg Cxg
Cxg
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Cxg
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Cxg
Cxg
Cxg
Cxg
Cxg
Cxg
CxgCxgCxg
Cxg
Cxg
Cxg
Cxg
CxgCxg
Cxg Cxg
Ci
Ci
Ci
CiCi
Ci
Ci
Ci
Ci
Ci
Ci
Ci
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Ci
CiCi
Ci
Ci
Ci
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Ci
Ci
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Ci
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Ci
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Ci
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Ci
Ci
Ci
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A
A'
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B
C'
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D'
D
E'
E
F'
F
G
G'
H
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