Earth and Planetary Science Letters

Isotopic evidence from an Antarctic carbonaceous chondrite for two reaction pathways of extraterrestrial PAH formation
pp. 1-7(7)
Authors: Naraoka^a H.; Shimoyama^b A.; Harada^b K.

Anatomy of black veins in Zagami: clues to the formation of high-pressure phases
pp. 37-55(19)
Authors: Langenhorst F.; Poirier¹ J.-P.

¹⁶O enrichments in aluminum-rich chondrules from ordinary chondrites
pp. 57-74(18)
Authors: Russell^a S.S.; MacPherson^a G.J.; Leshin^b1 L.A.; McKeegan^b K.D.

Zr isotope anomalies in chondrites and the presence of ⁹²Nb in the early solar system
pp. 75-81(7)
Authors: Sanloup C.; Blichert-Toft J.; Telouk P.; Gillet P.; Albarede F.

¹⁸²Hf-¹⁸²W systematics in eucrites: the puzzle of iron segregation in the early solar system
pp. 83-94(12)
Authors: Quitte G.; Birck J.-L.; Allegre C.J.

The origin of the depletions of V, Cr and Mn in the mantles of the Earth and Moon
pp. 95-107(13)
Authors: Gessmann C.K.; Rubie D.C.

A new astronomical timescale for the loess deposits of Northern China
pp. 125-139(15)
Authors: Heslop D.; Langereis C.G.; Dekkers M.J.

High absolute paleointensity during a mid Miocene excursion of the Earth's magnetic field
pp. 141-154(14)
Authors: Leonhardt^a R.; Hufenbecher^a F.; Heider^b F.; Soffel^a H.C.

Paleomagnetic study of French Guyana Early Jurassic dolerites: hypothesis of a multistage magmatic event
pp. 155-168(14)
Authors: Nomade^a S.; Theveniaut^b H.; Chen^a Y.; Pouclet^a A.; Rigollet^a C.

Cooling behaviour of partial thermoremanences induced in multidomain magnetite
pp. 169-179(11)
Author: Muxworthy A.R.

Modelling the emplacement of compound lava flows
pp. 181-197(17)
Authors: Blake S.; Bruno¹ B.C.

Effect of phyllosilicates on fluid-assisted healing of gouge-bearing faults
pp. 199-210(12)
Authors: Bos B.; Spiers C.J.

Giant quartz vein systems in accretionary orogenic belts: the evidence for a metamorphic fluid origin from ¹⁵N and ¹³C studies
pp. 211-224(14)
Authors: Jia Y.; Kerrich R.

U-Pb single-grain dating of detrital zircon in the Cambrian of central Poland: implications for Gondwana versus Baltica provenance studies
pp. 225-240(16)
Authors: Valverde-Vaquero^a P.; Dorr^a W.; Belka^b Z.; Franke^a W.; Wiszniewska^c J.; Schastok^a J.

Hydrothermal plumes above the East Scotia Ridge: an isolated high-latitude back-arc spreading centre
pp. 241-250(10)
Authors: German^a C.R.; Livermore^b R.A.; Baker^c E.T.; Bruguier^b N.I.; Connelly^a D.P.; Cunningham^b A.P.; Morris^b P.; Rouse^a I.P.; Statham^a P.J.; Tyler^a P.A.

Oxygen isotope evidence for the origin of chemical variations in lavas from Theistareykir volcano in Iceland's northern volcanic zone
pp. 269-286(18)
Authors: Eiler^a J.M.; Gronvold^b K.; Kitchen^a N.

Topography and isotherms revisited: the influence of laterally migrating drainage divides
pp. 287-303(17)
Authors: Stuwe^a K.; Hintermuller^b M.

Methane-related authigenic carbonates of eastern Mediterranean Sea mud volcanoes and their possible relation to gas hydrate destabilisation
pp. 321-338(18)
Authors: Aloisi^a G.; Pierre^a C.; Rouchy^b J.-M.; Foucher^c J.-P.; Woodside^d J.; the MEDINAUT Scientific Party

Critical comment on: A.J. Mory et al. 'Woodleigh, Carnarvon Basin, Western Australia: a new 120 km diameter impact structure'
pp. 353-357(5)
Authors: Reimold^a W.U.; Koeberl^b C.

Response to 'Critical comment on A.J. Mory et al., 2000, Woodleigh, Carnarvon Basin, Western Australia: a new 120 km diameter impact structure' by W.U. Reimold and C. Koeberl
pp. 359-365(7)
Authors: Mory^a A.J.; Iasky^a R.P.; Glikson^b A.Y.; Pirajno^a F.