Energetic particle injections from Earth's magnetotail-characterized as the sudden flux enhancements of tens to hundreds of keV electrons and/or ions-are one of fundamental signatures of substorm activity in the inner magnetosphere. Fractions of the injected electrons and ions play an important role in building-up Earth's ring current during magnetic storms, providing the seed population for MeV electrons in the outer radiation belt, and introducing the source population responsible for the generation and growth of various plasma waves. How the particles of different species/energies can be transported and/or energized and what controls the penetration of injections inside geosynchronous orbit (GEO) where the magnetic field intensity becomes much stronger are a subject of ongoing debate. The dispersionless character of the flux enhancements-so-called dispersionless injection-is known as a manifestation of the particles that are undergoing either a local energization process or a rapid transport process, or both at/near the leading edge of injections (injection region). In other words, a spacecraft at/near the injection region itself should observe a dispersionless injection, and such in situ measurements would provide an opportunity to understand the underlying mechanisms responsible for the injection.Dispersionless injections are categorized into three types: both-species injections (i.e., coincident injections of both ions (mainly protons, H + ) and electrons (e -)), e --only injections, and H + -only injections. Early energetic particle observations from a LANL spacecraft at GEO provided a statistical picture for the three types of dispersionless injections to occur with local time (or spatial) offsets with respect to midnight (Birn et al., 1997;Thomsen et al., 2001). That is, the e --only (H + -only) injections are preferentially observed ∼2 h after (∼3 h before) local midnight, while the both-species injections occur around midnight. The spatially dependent pattern of the three types has been explained in terms of H + and einjection boundaries that have a dawn-dusk separation and move earthward quasi-stationarily.