The rif belt
A Chalouan, A Michard, KE Kadiri, F Negro… - … evolution: the geology …, 2008 - Springer
The Rif Belt belongs to a much larger orogen, ie the Betic-Rif-Tell orogen, which itself is part
of the still larger Mediterranean Alpine belts (Fig. 5.1; see also Chap. 1.1, Fig. 1.2). The Rif …
of the still larger Mediterranean Alpine belts (Fig. 5.1; see also Chap. 1.1, Fig. 1.2). The Rif …
Active mud volcanism in the West Alboran Basin: Geochemical evidence of hydrocarbon seepage
VN Blinova, MC Comas, MK Ivanov… - Marine and Petroleum …, 2011 - Elsevier
The West Alboran Basin was previously classified as a mud volcanic province consisting of
two mud volcano (MV) fields that are inactive at the present day: the Northern (Spanish) and …
two mud volcano (MV) fields that are inactive at the present day: the Northern (Spanish) and …
[PDF][PDF] El Messiniense en el Golfo de Valencia y el Mar de Alborán: implicaciones paleogeográficas y paleoceanográficas
WM del Olmo - Revista de la Sociedad Geológica de España, 2011 - sge.usal.es
En el Golfo de Valencia y el Mar de Alborán el tiempo Messiniense está distribuido en tres
Secuencias Deposicionales de edades Tortoniense superior-Messiniense inferior …
Secuencias Deposicionales de edades Tortoniense superior-Messiniense inferior …
Origin of lipid biomarkers in mud volcanoes from the Alboran Sea, western Mediterranean
C López-Rodríguez, A Stadnitskaia… - …, 2014 - bg.copernicus.org
Mud volcanoes (MVs) are the most prominent indicators of active methane/hydrocarbon
venting at the seafloor on both passive and active continental margins. Their occurrence in …
venting at the seafloor on both passive and active continental margins. Their occurrence in …
[PDF][PDF] Spatial modelling and risk assessment of Sidoarjo mud volcanic flow
R Rifai - 2008 - itc.nl
On 29 May 2006 mud volcano occurred in Sidoarjo-East Java 23 km south of Surabaya. This
is a geological phenomenon due to over-pressurized sub-surface mud layers. This mud …
is a geological phenomenon due to over-pressurized sub-surface mud layers. This mud …
Грязевой вулканизм Средиземного, Черного и Каспийского морей: специфика развития и проявления
ЕФ Шнюков, АА Алиев, РР Рахманов - Геология и полезные …, 2017 - cyberleninka.ru
Рассмотрены ареалы развития, количественное распределение, морфометрия
грязевых вулканов Средиземного, Черного и Каспийского морей, время их заложения …
грязевых вулканов Средиземного, Черного и Каспийского морей, время их заложения …
[PDF][PDF] Estructura y evolución durante el Mioceno del diapirismo de lodo en el sector septentrional de la Cuenca Oeste de Alborán (Mediterráneo occidental)
El diapirismo y volcanismo de lodo se originan en el depocentro mayor de la Cuenca del
Mar de Alborán (la Cuenca Oeste de Alborán, COA, con espesor de sedimentos> 8 km) a …
Mar de Alborán (la Cuenca Oeste de Alborán, COA, con espesor de sedimentos> 8 km) a …
Ye. F. Shnyukov, Ad. A. Aliyev, RR Rahmanov. MUD VOLCANISM OF MEDITERRANEAN, BLACK AND CASPIAN SEAS: SPECIFICITY OF DEVELOPMENT AND …
YF Shnyukov - gpimo.nas.gov.ua
In the article authors are considered development areas, quantitative distribution,
morphometry of mud volcanoes of the Mediterranean, Black and Caspian seas, time of their …
morphometry of mud volcanoes of the Mediterranean, Black and Caspian seas, time of their …
[引用][C] SPATIAL MODELING AND ELEMENTS AT RISK ASSESSMENT OF SIDOARJO MUD VOLCANIC FLOW
EATR ASSESSMENT