ABSTRATU
Timor Leste forma liu husi fenomenu jeolójiku, husi plaka tektonika, Euro Asiatiku ho Indo-Australia halo subdaksaun hodi forma illa timor ho komppleksu tebes husi variedade litoestratigrafia iha área estudu husi unidade litolojia idade hahu forma iha área estudu peskizador nota katak hahu forma iha periodu permiku forma unidade litolojia kalkarenitu, kontinua mai iha jurasiku hahu forma unidade litolojia kalsilutitu no iha miosen okos forma unidade litolojia breksia kalkariu mai iha miosen leten no halo diapireme hodi forma Bobonaru scla clay. Jeolojikamente kondisaun jeolójiku liu husi aspektu jeomorfolojia forma iha área estudu prosesu endojeniku ho eksojeniku. Determinasaun iha área estudu husi unidade jeomorfolojia estrutural kuaze iha mapa área peskiza 35%, denundasional 40% no fluvial 25%. Liu husi unidade litoestratigrafia arjilitu 45%, breksia kalkariu, 15% kalsilutit 15% no kalkarenitu 35%. Tuir observasaun iha area estudu forsa detensaun jeralmente mai husi SW/NE. Amostra arjila teste iha laboratorium bazeia ba liquid limit, plastis limit no indeks limit, rezultadu hatudu katak plastidu ki'ik to bo'ot, husi plastiadu ne'e bo'ot tempu udan halo movimentu rai ka erozaun. Analiza ba elementos kimika liu husi XRF (X-Ray Fluoresence) hodi hatene persentajen husi mineral kada (pontu parajen) husi amostra nebe iha P.p. 227 husi mineral fero (Fe) 1,18%, P.p. 170 persentajen mineral fero (Fe) 2,46 no P.p. 101 persentajen mineral (Fe) 3,81%. Lifuan Xave: Timor Leste, Mapamentu, Jeolojia, Jeomorfolojia, Estudu



ABSTRACT Timor-Leste is made up of the geological phenomenon, from plaque, Euro and the Indo-Pacific of Australia, by subduing the Timorese island, with a full force of a gouggish plant in the study area of the coastline since its study area in the study area, noting that it started in the period allowing a mobile theychiatric unit to be formed, but it is continuing to form unit under the ocean and in the ocean to form a quistic unit under the ocean in the ocean. Geologically the geologica conditions through the geology aspects of the endomiological process study area with macro scope. Determination in the area of geomorphological units is almost entirely based on the survey area 35%, 40% denunciation and fluvial 25%. Through a wheel unit of 45%, brief cartographic discretion, 15% of underpants 15% and 35%. According to observations in the study of detention forces generally come from SW/NE. Samples of testing in laboratory based on liquid, plastic limit and index, the results show that plastic is small to large, from plastic is large during the rainy season, causing land movement or erosion. Analysis of the composite elements of XRF (X-Ray Fluoresence) to understand the percentage of mineral each sample in P.p. 227 of mineral deficit (Fe) 1,18%, P. 170 percentage mineral fero (Fe) 2,46 and p.101 percentage mineral (Fe) 3,81%. Keywords: East Timor, Mapping, Geology, Geomorfology, Estud