I've successfully copied the files from these folders to a thumb drive and moved them to a new computer. Note that part of the registration information is the local computer name, so in order to work on a different machine (or a clean Windows install on the same machine) the computer name needs to stay the same. Just name the computer the same, copy the .slip files to the same location on the new machine, and then install Delphi/RAD Studio.
activation file delphi 2010 .slip 11
I had a similar problem when renaming my Windows 10 computer. Apparently the license is bound to the computer name. I had to re-register Delphi after renaming my computer but failed because of the limit of my license key.Solution was renaming back my computer and renaming C:\ProgramData\Embarcadero\.cgb_license.corrupted and C:\ProgramData\Embarcadero\.licenses\.cg_license.corrupted to files without the .corrupted as suffix. My licence slip file was C:\ProgramData\Embarcadero\.2016_2.#############.slip.
I had a similar problem when renaming my Windows 10 computer. Apparently the license is bound to the computer name. I had to re-register Delphi after renaming my computer but failed because of the limit of my license key. Solution was renaming back my computer and renaming C:\ProgramData\Embarcadero\.cgb_license.corrupted and C:\ProgramData\Embarcadero\.licenses\.cg_license.corrupted to files without the .corrupted as suffix. My licence slip file was C:\ProgramData\Embarcadero\.2016_2.#############.slip.
A. This error is caused when an activation file (reg*.txt) or slip file (*.slip) file is found in the same directory as the installer and does not apply to the current installation. To resolve the problem copy the installer to a new folder which contains no other files.
After a bit more digging around on the internets, I found a reference to the location of some other .slip files, in ProgramData\Embarcadero (I can only think that the one in the License folder of the installation itself is just there for decoration?)
Oh well, at least what should have taken 30 seconds or a couple of minutes, at most, only took the best part of TWO HOURS! (Now that I know about those additional .slip files, it will be much quicker next time of course, as it will be for you, dear reader ? ).
Volkswagen Group of America, Inc. (Volkswagen) is recalling certain model year 2009-2010 Volkswagen Jetta A5 Sedan, 2009 Volkswagen Jetta SportWagen, Eos, GTI, Rabbit and Audi A3 vehicles, and 2010 Volkswagen Golf A6 vehicles. The Antilock Brake System (ABS) control unit may fail during ABS or Electronic Stability Control (ESC) activation, possibly causing a loss of vehicle control.
The 2004 Sumatra-Andaman Mw9.3 and the 2011 Tohoku (Japan) Mw9.0 earthquakes and tsunamis were huge geological events with major societal consequences. Both were along subduction boundaries and ruptured portions of these boundaries that had been deemed incapable of such events. Submarine strike-slip earthquakes, such as the 2010 Mw7.0 in Haiti, are smaller but may be closer to population centers and can be similarly catastrophic. Both classes of earthquakes remobilize sediment and leave distinct signatures in the geologic record by a wide range of processes that depends on both environment and earthquake characteristics. Understanding them has the potential of greatly expanding the record of past earthquakes, which is critical for geohazard analysis. Recent events offer precious ground truth about the earthquakes and short-lived radioisotopes offer invaluable tools to identify sediments they remobilized. In the 2011 Mw9 Japan earthquake they document the spatial extent of remobilized sediment from water depths of 626m in the forearc slope to trench depths of 8000m. Subbottom profiles, multibeam bathymetry and 40 piston cores collected by the R/V Natsushima and R/V Sonne expeditions to the Japan Trench document multiple turbidites and high-density flows. Core tops enriched in xs210Pb,137Cs and 134Cs reveal sediment deposited by the 2011 Tohoku earthquake and tsunami. The thickest deposits (2m) were documented on a mid-slope terrace and trench (4000-8000m). Sediment was deposited on some terraces (600-3000m), but shed from the steep forearc slope (3000-4000m). The 2010 Haiti mainshock ruptured along the southern flank of Canal du Sud and triggered multiple nearshore sediment failures, generated turbidity currents and stirred fine sediment into suspension throughout this basin. A tsunami was modeled to stem from both sediment failures and tectonics. Remobilized sediment was tracked with short-lived radioisotopes from the nearshore, slope, in fault basins including the
2ff7e9595c
Comments