A global survey of the stable isotope and chemical compositions of bottled and canned beers as a guide to authenticity

Stable isotope and trace metal compositi

Stable isotope and trace metal compositions of Australian prawns as a guide to authenticity and wholesomeness

✍ Carter, J.F.; Tinggi, U.; Yang, X.; Fry, B. 📂 Article 📅 2015 🏛 Elsevier Science 🌐 English ⚖ 421 KB

Using variation in the chemical and stab

Using variation in the chemical and stable isotopic composition of Zostera noltii to assess nutrient dynamics in a temperate seagrass meadow

✍ S. Papadimitriou; H. Kennedy; R.M.N.V. Rodrigues; D.P. Kennedy; T.H.E. Heaton 📂 Article 📅 2006 🏛 Elsevier Science 🌐 English ⚖ 368 KB

Comment to “Chlorine stable isotopes and

Comment to “Chlorine stable isotopes and halogen concentrations in convergent margins with implications for the Cl isotopes cycle in the ocean” by Wei et al. A review of the Cl isotope composition of serpentinites and the global chlorine cycle

✍ Z.D. Sharp; J.D. Barnes 📂 Article 📅 2008 🏛 Elsevier Science 🌐 English ⚖ 273 KB

The global network of plate boundaries c

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.

✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin