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<md:lastName>Jones</md:lastName>
<md:firstName>E J W</md:firstName>
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<md:lastName>Laughton</md:lastName>
<md:firstName>Anthony S</md:firstName>
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<md:author id="dataset.author56871">
<md:lastName>Hill</md:lastName>
<md:firstName>M N</md:firstName>
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<md:lastName>Davies</md:lastName>
<md:firstName>D</md:firstName>
<md:orcid>0000-0001-6304-3938</md:orcid>
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<md:year>1966</md:year>
<md:title>Annotated record of the detailed examination of Mn deposits from the Madcap Volcano in the Madeira-Cape Verde Abyssal plain</md:title>
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<md:URI>https://doi.org/10.1594/PANGAEA.874690</md:URI>
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<md:lastName>Jones</md:lastName>
<md:firstName>E J W</md:firstName>
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<md:lastName>Laughton</md:lastName>
<md:firstName>Anthony S</md:firstName>
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<md:author id="ref90472.author56871">
<md:lastName>Hill</md:lastName>
<md:firstName>M N</md:firstName>
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<md:lastName>Davies</md:lastName>
<md:firstName>D</md:firstName>
<md:orcid>0000-0001-6304-3938</md:orcid>
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<md:year>1976</md:year>
<md:title>A geophysical study of part of the western boundary of the Madeira-Cape Verde Abyssal plain</md:title>
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<md:source id="ref90472.journal16769" relatedTermIds="33974,34022" type="journal">Deep Sea Research and Oceanographic Abstracts</md:source>
<md:volume>13(5)</md:volume>
<md:URI>https://doi.org/10.1016/0011-7471(76)90909-8</md:URI>
<md:pages>889-907</md:pages>
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<md:abstract>The results are discussed of a geophysical survey undertaken by R.R.S. Discovery II early in 1962 in an area centred on 29° 15'N, 25° 5'W at the western extremity of the Madeira-Cape Verde Abyssal Plain. Seismic investigations show that the sediments are underlain by an intermediate layer about 2 km in thickness of velocity 4.1-5.4 km/sec which overlies a deep layer 5.2-km thick of velocity 6.3-6.8 km/sec. Refracted arrivals on the longest seismic line give a depth of 13.2 km to the M discontinuity.
Magnetic results indicate that the topography of the abyssal hills in the western part of the area is probably continued eastwards as sub-bottom relief beneath the sediments of the abyssal plain. They also support the hypothesis that the intermediate seismic layer (layer 2) is composed predominantly of volcanic rocks. Examination of a well-defined magnetic anomaly over one topographic feature ("The Madcap Volcano") shows it to be composed of magnetized rocks (I = 8.4 × 10**-3 e.m.u./cm**3) having a direction of magnetization which points upwards at 25° with an azimuth of 305°. Measurements at ten heat flow stations show that the average geothermal flux in this region is 1.20 (±0.11) µcal/cm**2/sec.</md:abstract>
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<md:lastName>Moore</md:lastName>
<md:firstName>Carla J</md:firstName>
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<md:lastName>Alameddin</md:lastName>
<md:firstName>George</md:firstName>
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<md:lastName>Chen</md:lastName>
<md:firstName>Kuiying</md:firstName>
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<md:author id="ref67195.author53901">
<md:lastName>Barton</md:lastName>
<md:firstName>Mark</md:firstName>
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<md:year>1992</md:year>
<md:title>The NOAA and MMS Marine Minerals Geochemical Database</md:title>
<md:source>National Geophysical Data Center, NOAA</md:source>
<md:URI>https://doi.org/10.7289/V52Z13FT</md:URI>
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<md:lastName>Warnken</md:lastName>
<md:firstName>Robin R</md:firstName>
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<md:lastName>Virden</md:lastName>
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<md:lastName>Moore</md:lastName>
<md:firstName>Carla J</md:firstName>
<md:eMail>carla.j.moore@noaa.gov</md:eMail>
<md:orcid>0000-0002-2610-8648</md:orcid>
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<md:year>1992</md:year>
<md:title>The NOAA and MMS Marine Minerals Bibliography</md:title>
<md:source>National Geophysical Data Center, NOAA</md:source>
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<md:comment>From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.</md:comment>
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