In this work a detailed geological map of the graphite mineralizations of the Aracena Metamorphic Belt (SW Iberian Massif) is shown. Three types of mineralizations have been distinguished according to lithostratigraphic and structural criteria: 1) Stratiform deposits related to gneissic lenticular bodies embedded within a complex calc-silicate sequence 2)Veinlets of graphite cutting across mafic granulites; and 3) Disseminated graphite within gneisses and quartzites belonging to the Fuente del Oro series. Only the first type of mineralizations could have an economic interest.DGICYT. Gobierno de España-PB93-006
D etailed geological mapping o f the granitoids that make this part o f Central Extremadura ( A lb a...
The degree of metamorphism affecting the Devonian-Carboniferous rocks of the Palaeozoic Cinco Villas...
Probably Lower Paleozoic quartzo-pelitic schists with bands of feldspathic schists, white and black ...
In this work a detailed geological map o f the graphite mineralizations of the Aracena Metamorphic B...
Four distinct associations of graphite have been identified in the low-pressure, high-temperature be...
Several late leucogranite small plutons appear in the high grade zone of the continental domain (CD)...
Graphite is found dispersed in high-grade metapelitic rocks of the Anatectic Complex of Toledo (ACT)...
We have investigated volcanic-rock-hosted graphitem in eralization in the Huelma area of the Betic C...
O Distrito Grafitífero Aracoiába-Baturité apresenta depósitos do tipo gnaisse grafitoso (minério dis...
The structural analysis of marbles from the Aracena metamorphic belt has proven to be very useful to...
Graphite is found dispersed in high-grade metapelitic rocks of the Anatectic Complex of Toledo 15 (A...
The crystalline core of the Hercynian Orogen in N.W. Iberia contains five allochthonous, polymetamor...
A review is given of pre-hercynian metasediments and granites (including per-alkaline aegirineriebec...
Talc mineralization related to the ultramafic bodies of the Río de Las Tunas belt, Frontal Cordiller...
The area around Santiago de Compostela has been subjected to petrological and structural investigati...
D etailed geological mapping o f the granitoids that make this part o f Central Extremadura ( A lb a...
The degree of metamorphism affecting the Devonian-Carboniferous rocks of the Palaeozoic Cinco Villas...
Probably Lower Paleozoic quartzo-pelitic schists with bands of feldspathic schists, white and black ...
In this work a detailed geological map o f the graphite mineralizations of the Aracena Metamorphic B...
Four distinct associations of graphite have been identified in the low-pressure, high-temperature be...
Several late leucogranite small plutons appear in the high grade zone of the continental domain (CD)...
Graphite is found dispersed in high-grade metapelitic rocks of the Anatectic Complex of Toledo (ACT)...
We have investigated volcanic-rock-hosted graphitem in eralization in the Huelma area of the Betic C...
O Distrito Grafitífero Aracoiába-Baturité apresenta depósitos do tipo gnaisse grafitoso (minério dis...
The structural analysis of marbles from the Aracena metamorphic belt has proven to be very useful to...
Graphite is found dispersed in high-grade metapelitic rocks of the Anatectic Complex of Toledo 15 (A...
The crystalline core of the Hercynian Orogen in N.W. Iberia contains five allochthonous, polymetamor...
A review is given of pre-hercynian metasediments and granites (including per-alkaline aegirineriebec...
Talc mineralization related to the ultramafic bodies of the Río de Las Tunas belt, Frontal Cordiller...
The area around Santiago de Compostela has been subjected to petrological and structural investigati...
D etailed geological mapping o f the granitoids that make this part o f Central Extremadura ( A lb a...
The degree of metamorphism affecting the Devonian-Carboniferous rocks of the Palaeozoic Cinco Villas...
Probably Lower Paleozoic quartzo-pelitic schists with bands of feldspathic schists, white and black ...