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Zhifeng Wan, Junsheng Luo, Xiaolu Yang, Wei Zhang, Jinqiang Liang, Lihua Zuo and Yuefeng Sun
Mud volcanoes and other fluid seepage pathways usually transport sufficient gas for the formation of gas reservoirs and are beneficial to the accumulation of gas hydrate. On the other hand, the fluid thermal effects of mud volcanoes can constrain the occ...
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Fabio Vittorio De Blasio
Mars has held large amounts of running and standing water throughout its history, as evidenced by numerous morphologies attributed to rivers, outflow channels, lakes, and possibly an ocean. This work examines the crater Antoniadi located in the Syrtis Ma...
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Gongzheng Ma, Linsen Zhan, Hailong Lu and Guiting Hou
Geological structure changes, including deformations and ruptures, developed in shallow marine sediments are well recognized but were not systematically reviewed in previous studies. These structures, generally developed at a depth less than 1000 m below...
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Anastasios Nikitas, Maria V. Triantaphyllou, Grigoris Rousakis, Ioannis Panagiotopoulos, Nikolaos Pasadakis, Ioannis Hatzianestis and Alexandra Gogou
This study presents the results derived from micropaleontological and organic geochemical analyses of mud breccia samples obtained (through gravity coring) from five mud volcanoes (Gelendzhik, Heraklion, Moscow, Milano, Leipzig) located at the Olimpi mud...
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Akira Ijiri, Koichi Iijima, Urumu Tsunogai, Juichiro Ashi and Fumio Inagaki
Clay mineralogy is an important characteristic of mud volcano sediments. This study determined the clay mineral compositions of sediment from two submarine mud volcanoes in the Kumano forearc basin, Nankai Trough, by X-ray diffraction analysis. Similar c...
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Agustawijaya, D.S.,Sukandi .
Pág. 100 - 109
Since the eruption of the Lusi Mud volcano in Sidoarjo, East Java, on May 2006, soil embankment dams have been built to keep hot mud within the ponds. Unfortunately, since the dams were sitting on poor weak ground, land subsidence intensively occurred ar...
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Maria Filomena Loreto, Umberta Tinivella, Flavio Accaino and Michela Giustiniani
A gas hydrate reservoir, identified by the presence of the bottom simulating reflector, is located offshore of the Antarctic Peninsula. The analysis of geophysical dataset acquired during three geophysical cruises allowed us to characterize this reservoi...
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Ricardo Thiele,Hugo Moreno,Sara Elgueta,Alfredo Lahsen,Sofia Rebolledo,M. Eugenia Petit-Breuilh
Pág. 229 - 253
The Quaternary geological history of the uppermost the Río Laja valley shows a complex interrelation between volcanic, mass wasting, and alluvial and fluvial sedimentary processes. The valley was initialiy carved by Lower Pleistocene glacial action on a ...
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Muhammad Burhannudinnur,Wildan Tri Koesmawardani
Pág. 196 - 205
The Mud Volcano System (SMV) is an interesting topic, especially the relatively shallow oil and gas basin in North East Java. The Tawun Formation is an alternating layer of claystone that is quite thick. It has been confirmed in several oil and gas field...
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