REFERENSI

· Barber, A.J., Tjokosapoetro, S., Charlton, T.R., 1986. Mud volcanoes, shale diapers,wrench faults andmelanges in accretionary complexes, eastern Indonesia. Am. Assoc. Pet. Geol. Bull. 70, 1729–1741.

· Bernard, B.B., Brooks, J.M., Sackett,W.M., 1978. Light hydrocarbons in recent Texas continental shelf and slope sediments. J. Geophys. Res. 83, 4053–4061.

· Brodsky, E.E., Roeloffs, E., Woodcock, D., Gall, I., M.M., 2003. A mechanism for sustained groundwater pressure changes induced by distant earthquakes. J. Geophys. Res. 108, 7.1–7.10.

· Chan, L.-H., Kastner, M., 2000. Lithium isotopic compositions of pore fluids and sediments in the Costa Rica subduction zone: implications for fluid processes and sediment contribution to the arc volcanoes. Earth Planet. Sci. Lett. 183, 275–290.

· Cita, M.B., Ivanov, M.K., Woodside, J.M., 1996. The Mediterranean Ridge Diapiric Belt, Special Issue. Mar. Geol. 132. 273 pp.

· Dahlmann, A., de Lange, G.J., 2003. Fluid-sediment interactions at Eastern Mediterranean mud volcanoes: a stable isotope study from ODP Leg 160. Earth Planet. Sci. Lett. 212, 377–391.

· Davies, R., Swarbrick, R., Evans, R., Huuse, M., 2007. Birth of a mud volcano: East Java, 29 May 2006. GSA Today 17, 4–9.

· Duan, Z., Sun, R., 2003. An improved model calculating CO2 solubility in pure water and aqueous NaCl solutions from 273 to 533 K and from 0 to 2000 bar. Chem. Geol. 193, 257–271.

· Egeberg, P.K., 1990. Unusual composition of pore waters found in the Izu-Bonin fore-arc sedimentary basin. Nature 344, 215–218.

· Elkhoury, J.E., Brodsky, E.E., Agnew, D.C., 2006. Seismic waves increase permeability. Nature 441, 1135–1138.

· Guliev, I.S., Feizullayev, A.A., 1997. All About Mud volcanoes. Nafta Press, Baku. 52 pp.

· Hensen, C., Wallmann, K., Schmidt, M., Ranero, C.R., Suess, E., 2004. Fluid expulsion related to mud extrusion off Costa Rica—a window to the subducting slab. Geology 32, 201–204.

· Hieke, W., 2004. The August 27, 1886 earthquake in Messenia (Peloponnesus) and reported flames over the Ionian Sea—a Mediterranean Ridge gas escape event? Mar. Geol. 207, 259–265.

· Hovland, M., Fichler, C., Rueslatten, H., Johansen, H., 2006. Deeprooted piercement structures in deep sedimentary basins— manifestations of supercritical water generation at depth? J. Geochem. Explor. 89, 157–160.

· Husen, S., Taylor, R., Smith, R.B., Heasler, H., 2004. Changes in geyser eruption behavior and remotely triggered seismicity in Yellowstone National Park produced by the 2002 M 7.9 Denali fault earthquake, Alaska. Geology 32, 537–540.

· Ishikawa, T., Nakamura, E., 1993. Boron isotope systematics of marine sediments. Earth Planet. Sci. Lett. 117, 567–580.

· Mazzini et al. / Earth and Planetary Science Letters 261 (2007) 375–388 387

· Ivanov, M.K., Limonov, A.F., van Weering, T.C.E., 1996. Comparative

· characteristics of the Black Sea and Mediterranean Ridge mud volcanoes. Mar. Geol. 132, 253–271.

· Jakubov, A.A., Ali-Zade, A.A., Zeinalov, M.M., 1971. Mud Volcanoes of the Azerbaijan SSR, Atlas (in Russian). Azerbaijan Academy of Sciences, Baku.

· Kholodov, V.N., 1983. Postsedimentary Transformations in Elisional Basins (example from Eastern Pre-Caucasus) (in Russian),150 pp.

· Kopf, A.J., 2002. Significance of mud volcanism. Rev. Geophys. 40, 1–52.

· Kusumastuti, A., Van Rensbergen, P., Warren, J.K., 2002. Seismic sequence analysis and reservoir potential of drowned Miocene carbonate platforms in the Madura Strait, East Java, Indonesia. Aapg Bull. 86, 213–232.

· Manga, M., Brodsky, E., 2006. Seismic triggering of eruptions in the far field: volcanoes and geysers. Annu. Rev. Earth Planet. Sci. 34, 263–291.

· Martin, B.M., Kastner, M., Henry, P., Le Pichon, X., Lallement, S., 1996. Chemical and isotopic evidence for sources of fluids in a mud volcano field seaward of the Barbados accretionary wedge. J Geophys. Res. 101, 20325–20345.

· Mau, S.,Rehder,G., Arroyo, I.G.,Gossler, J., Suess, E., 2007. Indications of a link between seismotectonics and CH4 release from seeps off Costa Rica. Geochem. Geophys. Geosyst. 8, 1–13.

· Mellors, R., Kilb, D., Aliyev, A., Gasanov, A., Yetirmishli, G., 2007. Correlations between earthquakes and large mud volcano eruptions. J. Geophys. Res. 112, B04304.

· Miller, S.A., Cristiano, C., Chiaraluce, L., Cocco, M., Barchi, M., Kaus, B.J.P., 2004. Aftershocks driven by a high-pressure CO2 source at depth. Nature 427, 724–727.

· Mukhtarov, A.S.h., Kadirov, F.A., Guliyev, I.S., Feyzullayev, A. Lerche, I., 2003. Temperature evolution in the Lokbatan mud volcano crater (Azerbaijan) after the eruption of 25 October 2001. Energy Explor. Exploit. 21, 187–207.

· Perry, E.A., Hower, J., 1972. Late-stage dehydration in deeply buried Pelitic sediments. Aapg Bull. 56, 2013–2021.

· Planke, S., Svensen, H., Hovland, M., Banks, D., Jamtveit, B., 2004. Mud and fluid migration in active mud volcanoes in Azerbaijan. Geo Mar. Lett. 23, 258–268.

· Schiller, D.M., Seubert, B.W., Musliki, S., Abdullah, M., 1994. The reservoir potential of globigerind sands in Indonesia. IPA 23^rd Annual Convention Proceedings, pp. 189–212.

· Tingay, M.R.P., Hillis, R.R., Morley, C.K., Swarbrick, R.E., Drake, S.J., 2005. Present-day stress orientation in Brunei: a snapshot of ‘prograding tectonics’ in the tertiary delta. J. Geol. Soc. 162, 39–49.

· U.S. Geological Survey, 200 http://earthquake.usgs.gov/eqcenter/ eqinthenews/2006/usneb6/.

· Walter, T.R.,Wang, R., Zimmer,M.,Grosser,H., Lühr,B., Ratdomopurbo, A., 2007. Volcanic activity influenced by tectonic earthquakes: static and dynamic stress triggering at Mt. Merapi. Geophys. Res. Lett. 34, L05304.

· Whiticar, M.J., 1999. Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane. Chem. Geol. 161, 291–314.

· Willumsen, P., Schiller, D.M., 1994. High quality volcaniclastic sandstone reservoirs in East Java, Indonesia. IPA 23rd Annual Convention Proceedings, pp. 101–111.

· Wilson, M.E.J., Bosence, D.W.J., Limbong, A., 2000. Tertiary syntectonic carbonate platform development in Indonesia. Sedimentology 47, 395–419. 388 A. Mazzini et al. / Earth and Planetary Science Letters 261 (2007) 375–388