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“I think people are skeptical about joining dating things.” A decade later, a somewhat savvier Zuckerberg has had a change of heart.

Last week, Facebook unveiled “Graph Search,” a new search engine that will allow users to comb through data from their existing online networks.

On the day of the announcement, the stock price of Inter Active Corp—the parent site of online dating behemoths —dropped by more than two per cent. Over the past two decades, the Internet has become a fixture of the modern-day romance plot.

In the early ’90s, just one per cent of new relationships began online.

(1996) Geochemistry of lavas from Mohns ridge, Norwegian-Greenland Sea: Implications for melting conditions and magma sources near Jan Mayen. G., Kingsley, R., Fontignie, D., Poreda, R., Xue, S. The hypothesised Mohns endmember, extrapolated to values that best explain available SMR samples as binary mixtures of Jan Mayen-Mohns Ridge lavas, has εPb = 15.43, and Hf, Nd, and Pb concentrations of 0.5, 3, and 0.3 ppm, respectively; mixtures of Jan Mayen and Kolbeinsey endmembers cannot fully explain NKR lava compositions. (2004) Volcanism on the Eggvin Bank (Central Norwegian-Greenland Sea, latitude similar to 71 degrees N): age, source, and relationship to the Iceland and putative Jan Mayen plumes. (b) Regional bathymetric map showing distribution of labelled seafloor features and Jan Mayen Island, with sample locations for this study from Jan Mayen Island (red), NKR (colours as in panel a), and SMR (orange).

Sticking around because you'd rather be with anyone than no one is a pretty unhealthy reason to prolong a relationship.

I have mine, too: an idealist and a bit of a romantic, I've been known to stay with a girl not because I really liked her but because I to really like her.

High (U) ratios measured in NKR lavas also require the presence of garnet in the melt source, indicating that the trace element compositions in Eggvin Bank basalts is principally controlled by mantle source composition. The data support lithologically and isotopically heterogeneous mantle source compositions for the Jan Mayen region and corroborate the existence of an Eggvin Bank end-member distinct from Jan Mayen mantle. Strontium isotopes were analyzed at the University of Wyoming by MC-ICP-MS (Thermo Finnigan Neptune Plus). (1999) Dispersion of the Jan Mayen and Iceland mantle plumes in the Arctic: A He-Pb-Nd-Sr isotope tracer study of basalts from the Kolbeinsey, Mohns, and Knipovich Ridges.

NKR basalts have elevated Pb and HREE compared to Jan Mayen Island and the MKR, indicating that they cannot be simple mixtures of Kolbeinsey-type and Jan Mayen-type magmas. for the Jan Mayen region, with symbols and references as in Figure 2. a 206Pb/204Pb, 207Pb/204Pb, 208Pb/204Pb, 176Hf/177Hf, and 143Nd/144Nd measured by MC-ICP-MS (Nu Plasma HR) at the Ecole Normale Supérieure de Lyon. G., Kingsley, R., Fontignie, D., Poreda, R., Xue, S.