Viện Vật lý địa cầu S u m m a r y. G ra v ity inverse problem s of 2D a n d 3D have been used by th e a u th o r for stu d y in g th e d e n sity m odel o f th e E a r th c ru st a n d adjoined to u p p e r M an tle b o u n d a ry in th e te rrito ry of V ietn am .
Some results of placura and granosa shells distribution in Nghe An regionOn the basis of placura placenta-arca granosa shells investigation in Quynh Van, Dien Chau and Nghi Tien, some new results can be made as the following:- Banks of placura placenta-arca granosa shells in Quynh Van and Nghi Tien; deep-seated in Quynh Nghia, DienChau and along Nghi Yen seashore have the time of 4000-4600 yr.- The appearance of the placura placenta-arca granosa shells banks have not either the sources from marinetransgression in Holocene, tectonic movement or artificial.- It is possible that those are the deposits of the natural geological activities courses to the seashore in the time of4000-4600 yr ago.
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