Original Articles U–Th–Pb monazite dating and the timing of arc–continent collision in East Timor
R. Berry, J. Thompson, S. Meffre & K. Goemann
Pages: 367-377 | DOI: 10.1080/08120099.2016.1217930
Widespread Neogene volcanism on Central Kerguelen Plateau, Southern Indian Ocean
R. A. Duncan, T. J. Falloon, P. G. Quilty & M. F. Coffin
Pages: 379-392 | DOI: 10.1080/08120099.2016.1221857
Epithermal and arc-related layered mafic platinum-group element mineralisation in the mafic–ultramafic rocks of eastern Papua
I. D. Lindley
Pages: 393-411 | DOI: 10.1080/08120099.2016.1212926
New age constraints on metamorphism, metasomatism and gold mineralisation at Plutonic Gold Mine, Marymia Inlier, Western Australia
M. F. Gazley, J. K. Vry, M.-A. Millet, M. R. Handler, E. du Plessis & J. A. Baker
Pages: 413-426 | DOI: 10.1080/08120099.2016.1212924
Integration of historic groundwater data into the Continent Scale Geochemistry initiative
D. J. Gray
Pages: 427-451 | DOI: 10.1080/08120099.2016.1218932
Lake George revisited: new evidence for the origin and evolution of a large closed lake, Southern Tablelands, NSW, Australia. 2: earliest Pleistocene (Gelasian) environments
M. Macphail, L. K. Fifield, B. Pillans & G. Hope
Pages: 453-468 | DOI: 10.1080/08120099.2016.1212399
Spatial distribution and temporal evolution of sediment transport pathway of deltaic deposits in a rift basin: an example from Liaodong Bay sub-basin, Bohai Bay, China
L. Jiang, S. H. Wu, Q. H. Yang, K. Huang, B. Yu, P. Wang & Z. H. Xu
Pages: 469-483 | DOI: 10.1080/08120099.2016.1217564
Tight-reservoir micropore formation and evolution in sedimentary organic-matter-bearing tuff: a case study from the Permian Tiaohu Formation in the Santanghu Basin, NW China
J. Ma & Z. Huang
Pages: 485-501 | DOI: 10.1080/08120099.2016.1219876
Physical and numerical simulations of the presence of a forsterite transitional zone at high temperature and pressure: insight for scCO2 geological storage
Z. Li, Y. Xu, L. Yang, J. Guo & J. Chen
Pages: 503-512 | DOI: 10.1080/08120099.2016.1217273
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