On the probable nature of magnetic anomalies in the Atlantic Rift Zone
An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
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| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1971 |
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| Reproduktion: |
Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 |
|---|---|
| Übergeordnetes Werk: |
in: Physics of the Earth and Planetary Interiors - Amsterdam : Elsevier, 4(1971), 5, Seite 381-405 |
| Übergeordnetes Werk: |
volume:4 ; year:1971 ; number:5 ; pages:381-405 |
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NLEJ180751921 |
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| 245 | 1 | 0 | |a On the probable nature of magnetic anomalies in the Atlantic Rift Zone |
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| 520 | |a An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. | ||
| 533 | |f Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 | ||
| 700 | 1 | |a Strakhov, V.N. |4 oth | |
| 700 | 1 | |a Lapina, M.I. |4 oth | |
| 700 | 1 | |a Mirlin, E.G. |4 oth | |
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(DE-627)NLEJ180751921 (DE-599)GBVNLZ180751921 DE-627 ger DE-627 rakwb eng On the probable nature of magnetic anomalies in the Atlantic Rift Zone 1971 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Strakhov, V.N. oth Lapina, M.I. oth Mirlin, E.G. oth in Physics of the Earth and Planetary Interiors Amsterdam : Elsevier 4(1971), 5, Seite 381-405 (DE-627)NLEJ180732102 (DE-600)1500666-9 0031-9201 nnns volume:4 year:1971 number:5 pages:381-405 http://linkinghub.elsevier.com/retrieve/pii/0031-9201(71)90021-5 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 4 1971 5 381-405 |
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(DE-627)NLEJ180751921 (DE-599)GBVNLZ180751921 DE-627 ger DE-627 rakwb eng On the probable nature of magnetic anomalies in the Atlantic Rift Zone 1971 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Strakhov, V.N. oth Lapina, M.I. oth Mirlin, E.G. oth in Physics of the Earth and Planetary Interiors Amsterdam : Elsevier 4(1971), 5, Seite 381-405 (DE-627)NLEJ180732102 (DE-600)1500666-9 0031-9201 nnns volume:4 year:1971 number:5 pages:381-405 http://linkinghub.elsevier.com/retrieve/pii/0031-9201(71)90021-5 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 4 1971 5 381-405 |
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(DE-627)NLEJ180751921 (DE-599)GBVNLZ180751921 DE-627 ger DE-627 rakwb eng On the probable nature of magnetic anomalies in the Atlantic Rift Zone 1971 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Strakhov, V.N. oth Lapina, M.I. oth Mirlin, E.G. oth in Physics of the Earth and Planetary Interiors Amsterdam : Elsevier 4(1971), 5, Seite 381-405 (DE-627)NLEJ180732102 (DE-600)1500666-9 0031-9201 nnns volume:4 year:1971 number:5 pages:381-405 http://linkinghub.elsevier.com/retrieve/pii/0031-9201(71)90021-5 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 4 1971 5 381-405 |
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(DE-627)NLEJ180751921 (DE-599)GBVNLZ180751921 DE-627 ger DE-627 rakwb eng On the probable nature of magnetic anomalies in the Atlantic Rift Zone 1971 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Strakhov, V.N. oth Lapina, M.I. oth Mirlin, E.G. oth in Physics of the Earth and Planetary Interiors Amsterdam : Elsevier 4(1971), 5, Seite 381-405 (DE-627)NLEJ180732102 (DE-600)1500666-9 0031-9201 nnns volume:4 year:1971 number:5 pages:381-405 http://linkinghub.elsevier.com/retrieve/pii/0031-9201(71)90021-5 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 4 1971 5 381-405 |
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(DE-627)NLEJ180751921 (DE-599)GBVNLZ180751921 DE-627 ger DE-627 rakwb eng On the probable nature of magnetic anomalies in the Atlantic Rift Zone 1971 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Strakhov, V.N. oth Lapina, M.I. oth Mirlin, E.G. oth in Physics of the Earth and Planetary Interiors Amsterdam : Elsevier 4(1971), 5, Seite 381-405 (DE-627)NLEJ180732102 (DE-600)1500666-9 0031-9201 nnns volume:4 year:1971 number:5 pages:381-405 http://linkinghub.elsevier.com/retrieve/pii/0031-9201(71)90021-5 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 4 1971 5 381-405 |
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An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. |
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An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. |
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An interpretation of magnetic surveys in the Atlantic Rift Zone is carried out using the method of analytic continuation of the field. The basic results are the following: (1)|Observed aeromagnetic fields are of complex interferential nature and of heterogeneous structure.(2)|When continued down to a depth of 1-2 km, there are no large ''non-disintegrating'' anomalies which might testify to the presence of large and homogeneously magnetized bodies at great depths.(3)|The ΔT"a field structure is to a great extent determined by the bottom depth.(4)|Local anomaly amplitudes decrease exponentially with increasing depth 4-6 times per km on the average.(5)|Linearity of anomalies is slightly expressed within our sectors; local anomalies do not correlate on the profiles.(6)|Field sources appear to be located close to the sea bottom- and they are extremely non-uniform. Normally and reversely magnetized bodies are present. |
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