\documentclass[11pt,twoside]{article}\makeatletter

\IfFileExists{xcolor.sty}%
  {\RequirePackage{xcolor}}%
  {\RequirePackage{color}}
\usepackage{colortbl}
\usepackage{wrapfig}
\usepackage{ifxetex}
\ifxetex
  \usepackage{fontspec}
  \usepackage{xunicode}
  \catcode`⃥=\active \def⃥{\textbackslash}
  \catcode`❴=\active \def❴{\{}
  \catcode`❵=\active \def❵{\}}
  \def\textJapanese{\fontspec{Noto Sans CJK JP}}
  \def\textChinese{\fontspec{Noto Sans CJK SC}}
  \def\textKorean{\fontspec{Noto Sans CJK KR}}
  \setmonofont{DejaVu Sans Mono}
  
\else
  \IfFileExists{utf8x.def}%
   {\usepackage[utf8x]{inputenc}
      \PrerenderUnicode{–}
    }%
   {\usepackage[utf8]{inputenc}}
  \usepackage[english]{babel}
  \usepackage[T1]{fontenc}
  \usepackage{float}
  \usepackage[]{ucs}
  \uc@dclc{8421}{default}{\textbackslash }
  \uc@dclc{10100}{default}{\{}
  \uc@dclc{10101}{default}{\}}
  \uc@dclc{8491}{default}{\AA{}}
  \uc@dclc{8239}{default}{\,}
  \uc@dclc{20154}{default}{ }
  \uc@dclc{10148}{default}{>}
  \def\textschwa{\rotatebox{-90}{e}}
  \def\textJapanese{}
  \def\textChinese{}
  \IfFileExists{tipa.sty}{\usepackage{tipa}}{}
\fi
\def\exampleFont{\ttfamily\small}
\DeclareTextSymbol{\textpi}{OML}{25}
\usepackage{relsize}
\RequirePackage{array}
\def\@testpach{\@chclass
 \ifnum \@lastchclass=6 \@ne \@chnum \@ne \else
  \ifnum \@lastchclass=7 5 \else
   \ifnum \@lastchclass=8 \tw@ \else
    \ifnum \@lastchclass=9 \thr@@
   \else \z@
   \ifnum \@lastchclass = 10 \else
   \edef\@nextchar{\expandafter\string\@nextchar}%
   \@chnum
   \if \@nextchar c\z@ \else
    \if \@nextchar l\@ne \else
     \if \@nextchar r\tw@ \else
   \z@ \@chclass
   \if\@nextchar |\@ne \else
    \if \@nextchar !6 \else
     \if \@nextchar @7 \else
      \if \@nextchar (8 \else
       \if \@nextchar )9 \else
  10
  \@chnum
  \if \@nextchar m\thr@@\else
   \if \@nextchar p4 \else
    \if \@nextchar b5 \else
   \z@ \@chclass \z@ \@preamerr \z@ \fi \fi \fi \fi
   \fi \fi  \fi  \fi  \fi  \fi  \fi \fi \fi \fi \fi \fi}
\gdef\arraybackslash{\let\\=\@arraycr}
\def\@textsubscript#1{{\m@th\ensuremath{_{\mbox{\fontsize\sf@size\z@#1}}}}}
\def\Panel#1#2#3#4{\multicolumn{#3}{){\columncolor{#2}}#4}{#1}}
\def\abbr{}
\def\corr{}
\def\expan{}
\def\gap{}
\def\orig{}
\def\reg{}
\def\ref{}
\def\sic{}
\def\persName{}\def\name{}
\def\placeName{}
\def\orgName{}
\def\textcal#1{{\fontspec{Lucida Calligraphy}#1}}
\def\textgothic#1{{\fontspec{Lucida Blackletter}#1}}
\def\textlarge#1{{\large #1}}
\def\textoverbar#1{\ensuremath{\overline{#1}}}
\def\textquoted#1{‘#1’}
\def\textsmall#1{{\small #1}}
\def\textsubscript#1{\@textsubscript{\selectfont#1}}
\def\textxi{\ensuremath{\xi}}
\def\titlem{\itshape}
\newenvironment{biblfree}{}{\ifvmode\par\fi }
\newenvironment{bibl}{}{}
\newenvironment{byline}{\vskip6pt\itshape\fontsize{16pt}{18pt}\selectfont}{\par }
\newenvironment{citbibl}{}{\ifvmode\par\fi }
\newenvironment{docAuthor}{\ifvmode\vskip4pt\fontsize{16pt}{18pt}\selectfont\fi\itshape}{\ifvmode\par\fi }
\newenvironment{docDate}{}{\ifvmode\par\fi }
\newenvironment{docImprint}{\vskip 6pt}{\ifvmode\par\fi }
\newenvironment{docTitle}{\vskip6pt\bfseries\fontsize{22pt}{25pt}\selectfont}{\par }
\newenvironment{msHead}{\vskip 6pt}{\par}
\newenvironment{msItem}{\vskip 6pt}{\par}
\newenvironment{rubric}{}{}
\newenvironment{titlePart}{}{\par }

\newcolumntype{L}[1]{){\raggedright\arraybackslash}p{#1}}
\newcolumntype{C}[1]{){\centering\arraybackslash}p{#1}}
\newcolumntype{R}[1]{){\raggedleft\arraybackslash}p{#1}}
\newcolumntype{P}[1]{){\arraybackslash}p{#1}}
\newcolumntype{B}[1]{){\arraybackslash}b{#1}}
\newcolumntype{M}[1]{){\arraybackslash}m{#1}}
\definecolor{label}{gray}{0.75}
\def\unusedattribute#1{\sout{\textcolor{label}{#1}}}
\DeclareRobustCommand*{\xref}{\hyper@normalise\xref@}
\def\xref@#1#2{\hyper@linkurl{#2}{#1}}
\begingroup
\catcode`\_=\active
\gdef_#1{\ensuremath{\sb{\mathrm{#1}}}}
\endgroup
\mathcode`\_=\string"8000
\catcode`\_=12\relax

\usepackage[a4paper,twoside,lmargin=1in,rmargin=1in,tmargin=1in,bmargin=1in,marginparwidth=0.75in]{geometry}
\usepackage{framed}

\definecolor{shadecolor}{gray}{0.95}
\usepackage{longtable}
\usepackage[normalem]{ulem}
\usepackage{fancyvrb}
\usepackage{fancyhdr}
\usepackage{graphicx}
\usepackage{marginnote}

\renewcommand{\@cite}[1]{#1}


\renewcommand*{\marginfont}{\itshape\footnotesize}

\def\Gin@extensions{.pdf,.png,.jpg,.mps,.tif}

  \pagestyle{fancy}

\usepackage[pdftitle={Molecular Zoning of Eocene and Miocene Age Deposits, North of Maracaibo Lake Basin},
 pdfauthor={}]{hyperref}
\hyperbaseurl{}

	 \paperwidth210mm
	 \paperheight297mm
              
\def\@pnumwidth{1.55em}
\def\@tocrmarg {2.55em}
\def\@dotsep{4.5}
\setcounter{tocdepth}{3}
\clubpenalty=8000
\emergencystretch 3em
\hbadness=4000
\hyphenpenalty=400
\pretolerance=750
\tolerance=2000
\vbadness=4000
\widowpenalty=10000

\renewcommand\section{\@startsection {section}{1}{\z@}%
     {-1.75ex \@plus -0.5ex \@minus -.2ex}%
     {0.5ex \@plus .2ex}%
     {\reset@font\Large\bfseries}}
\renewcommand\subsection{\@startsection{subsection}{2}{\z@}%
     {-1.75ex\@plus -0.5ex \@minus- .2ex}%
     {0.5ex \@plus .2ex}%
     {\reset@font\Large}}
\renewcommand\subsubsection{\@startsection{subsubsection}{3}{\z@}%
     {-1.5ex\@plus -0.35ex \@minus -.2ex}%
     {0.5ex \@plus .2ex}%
     {\reset@font\large}}
\renewcommand\paragraph{\@startsection{paragraph}{4}{\z@}%
     {-1ex \@plus-0.35ex \@minus -0.2ex}%
     {0.5ex \@plus .2ex}%
     {\reset@font\normalsize}}
\renewcommand\subparagraph{\@startsection{subparagraph}{5}{\parindent}%
     {1.5ex \@plus1ex \@minus .2ex}%
     {-1em}%
     {\reset@font\normalsize\bfseries}}


\def\l@section#1#2{\addpenalty{\@secpenalty} \addvspace{1.0em plus 1pt}
 \@tempdima 1.5em \begingroup
 \parindent \z@ \rightskip \@pnumwidth 
 \parfillskip -\@pnumwidth 
 \bfseries \leavevmode #1\hfil \hbox to\@pnumwidth{\hss #2}\par
 \endgroup}
\def\l@subsection{\@dottedtocline{2}{1.5em}{2.3em}}
\def\l@subsubsection{\@dottedtocline{3}{3.8em}{3.2em}}
\def\l@paragraph{\@dottedtocline{4}{7.0em}{4.1em}}
\def\l@subparagraph{\@dottedtocline{5}{10em}{5em}}
\@ifundefined{c@section}{\newcounter{section}}{}
\@ifundefined{c@chapter}{\newcounter{chapter}}{}
\newif\if@mainmatter 
\@mainmattertrue
\def\chaptername{Chapter}
\def\frontmatter{%
  \pagenumbering{roman}
  \def\thechapter{\@roman\c@chapter}
  \def\theHchapter{\roman{chapter}}
  \def\thesection{\@roman\c@section}
  \def\theHsection{\roman{section}}
  \def\@chapapp{}%
}
\def\mainmatter{%
  \cleardoublepage
  \def\thechapter{\@arabic\c@chapter}
  \setcounter{chapter}{0}
  \setcounter{section}{0}
  \pagenumbering{arabic}
  \setcounter{secnumdepth}{6}
  \def\@chapapp{\chaptername}%
  \def\theHchapter{\arabic{chapter}}
  \def\thesection{\@arabic\c@section}
  \def\theHsection{\arabic{section}}
}
\def\backmatter{%
  \cleardoublepage
  \setcounter{chapter}{0}
  \setcounter{section}{0}
  \setcounter{secnumdepth}{2}
  \def\@chapapp{\appendixname}%
  \def\thechapter{\@Alph\c@chapter}
  \def\theHchapter{\Alph{chapter}}
  \appendix
}
\newenvironment{bibitemlist}[1]{%
   \list{\@biblabel{\@arabic\c@enumiv}}%
       {\settowidth\labelwidth{\@biblabel{#1}}%
        \leftmargin\labelwidth
        \advance\leftmargin\labelsep
        \@openbib@code
        \usecounter{enumiv}%
        \let\p@enumiv\@empty
        \renewcommand\theenumiv{\@arabic\c@enumiv}%
	}%
  \sloppy
  \clubpenalty4000
  \@clubpenalty \clubpenalty
  \widowpenalty4000%
  \sfcode`\.\@m}%
  {\def\@noitemerr
    {\@latex@warning{Empty `bibitemlist' environment}}%
    \endlist}

\def\tableofcontents{\section*{\contentsname}\@starttoc{toc}}
\parskip0pt
\parindent1em
\def\Panel#1#2#3#4{\multicolumn{#3}{){\columncolor{#2}}#4}{#1}}
\newenvironment{reflist}{%
  \begin{raggedright}\begin{list}{}
  {%
   \setlength{\topsep}{0pt}%
   \setlength{\rightmargin}{0.25in}%
   \setlength{\itemsep}{0pt}%
   \setlength{\itemindent}{0pt}%
   \setlength{\parskip}{0pt}%
   \setlength{\parsep}{2pt}%
   \def\makelabel##1{\itshape ##1}}%
  }
  {\end{list}\end{raggedright}}
\newenvironment{sansreflist}{%
  \begin{raggedright}\begin{list}{}
  {%
   \setlength{\topsep}{0pt}%
   \setlength{\rightmargin}{0.25in}%
   \setlength{\itemindent}{0pt}%
   \setlength{\parskip}{0pt}%
   \setlength{\itemsep}{0pt}%
   \setlength{\parsep}{2pt}%
   \def\makelabel##1{\upshape ##1}}%
  }
  {\end{list}\end{raggedright}}
\newenvironment{specHead}[2]%
 {\vspace{20pt}\hrule\vspace{10pt}%
  \phantomsection\label{#1}\markright{#2}%

  \pdfbookmark[2]{#2}{#1}%
  \hspace{-0.75in}{\bfseries\fontsize{16pt}{18pt}\selectfont#2}%
  }{}
      \def\TheFullDate{2019-01-15 (revised: 15 January 2019)}
\def\TheID{\makeatother }
\def\TheDate{2019-01-15}
\title{Molecular Zoning of Eocene and Miocene Age Deposits, North of Maracaibo Lake Basin}
\author{}\makeatletter 
\makeatletter
\newcommand*{\cleartoleftpage}{%
  \clearpage
    \if@twoside
    \ifodd\c@page
      \hbox{}\newpage
      \if@twocolumn
        \hbox{}\newpage
      \fi
    \fi
  \fi
}
\makeatother
\makeatletter
\thispagestyle{empty}
\markright{\@title}\markboth{\@title}{\@author}
\renewcommand\small{\@setfontsize\small{9pt}{11pt}\abovedisplayskip 8.5\p@ plus3\p@ minus4\p@
\belowdisplayskip \abovedisplayskip
\abovedisplayshortskip \z@ plus2\p@
\belowdisplayshortskip 4\p@ plus2\p@ minus2\p@
\def\@listi{\leftmargin\leftmargini
               \topsep 2\p@ plus1\p@ minus1\p@
               \parsep 2\p@ plus\p@ minus\p@
               \itemsep 1pt}
}
\makeatother
\fvset{frame=single,numberblanklines=false,xleftmargin=5mm,xrightmargin=5mm}
\fancyhf{} 
\setlength{\headheight}{14pt}
\fancyhead[LE]{\bfseries\leftmark} 
\fancyhead[RO]{\bfseries\rightmark} 
\fancyfoot[RO]{}
\fancyfoot[CO]{\thepage}
\fancyfoot[LO]{\TheID}
\fancyfoot[LE]{}
\fancyfoot[CE]{\thepage}
\fancyfoot[RE]{\TheID}
\hypersetup{citebordercolor=0.75 0.75 0.75,linkbordercolor=0.75 0.75 0.75,urlbordercolor=0.75 0.75 0.75,bookmarksnumbered=true}
\fancypagestyle{plain}{\fancyhead{}\renewcommand{\headrulewidth}{0pt}}

\date{}
\usepackage{authblk}

\providecommand{\keywords}[1]
{
\footnotesize
  \textbf{\textit{Index terms---}} #1
}

\usepackage{graphicx,xcolor}
\definecolor{GJBlue}{HTML}{273B81}
\definecolor{GJLightBlue}{HTML}{0A9DD9}
\definecolor{GJMediumGrey}{HTML}{6D6E70}
\definecolor{GJLightGrey}{HTML}{929497} 

\renewenvironment{abstract}{%
   \setlength{\parindent}{0pt}\raggedright
   \textcolor{GJMediumGrey}{\rule{\textwidth}{2pt}}
   \vskip16pt
   \textcolor{GJBlue}{\large\bfseries\abstractname\space}
}{%   
   \vskip8pt
   \textcolor{GJMediumGrey}{\rule{\textwidth}{2pt}}
   \vskip16pt
}

\usepackage[absolute,overlay]{textpos}

\makeatother 
      \usepackage{lineno}
      \linenumbers
      
\begin{document}

             \author[1]{Eng. Jhoan Jose Urdaneta M.  Sc.}

\renewcommand\Authands{ and }

\date{\small \em Received: 6 December 2018 Accepted: 1 January 2019 Published: 15 January 2019}

\maketitle


\begin{abstract}
        


The purpose of this research is to document the molecular zoning of trapped crudes in La Rosa Basal Formation (BLR) / Arenas B, located in Block I, in the West of the Bolivarian Republic of Venezuela, specifically in the Lake Maracaibo Basin, in areas VLA0016 and VLA0033 of the Lagomar Production Unit. For the development of this study, a collection of the crude samples in the field following the standard methodology was carried out. Then, at the laboratory level, the atomic relationships between compounds were determined to establish the physicalchemical transformation of the organic material from its deposition to their current state.

\end{abstract}


\keywords{fingerprint, biomarkers, pristane, phytane, star diagram}

\begin{textblock*}{18cm}(1cm,1cm) % {block width} (coords) 
\textcolor{GJBlue}{\LARGE Global Journals \LaTeX\ JournalKaleidoscope\texttrademark}
\end{textblock*}

\begin{textblock*}{18cm}(1.4cm,1.5cm) % {block width} (coords) 
\textcolor{GJBlue}{\footnotesize \\ Artificial Intelligence formulated this projection for compatibility purposes from the original article published at Global Journals. However, this technology is currently in beta. \emph{Therefore, kindly ignore odd layouts, missed formulae, text, tables, or figures.}}
\end{textblock*}


\let\tabcellsep& 	 	 		 
\section[{Introduction}]{Introduction}\par
he Maracaibo Lake Basin has the most economically important oil fields for the Western Venezuelan Region, which are composed of several wells that produce oil from deposits located at different stratigraphic levels of Cretaceous and tertiary age. The data and samples that were analyzed and studied were sampled at the wellhead, using the methodology learned from the Zuliano Institute of Technological Research (INZIT).\par
The results obtained from these analyzes allowed to show the presence of crude oils with different geochemical characteristics indicating the origin of organic matter, depositional environment, degree of maturity, API gravity and the possibility of several alteration processes within the reservoir. Among the main processes of degradation of an oil can be mentioned: biodegradation, water washing, thermal alteration, among others. Also, the differences detected would point to a lack of communication between several compartments that have been isolated between them and, consequently, have followed different lines of structural and compositional evolution.\par
Finally, the molecular parameters of the crude oils of interest were determined, through analysis of biomarkers extracted from crude oil by gas chromatography coupled to mass spectrometry, this in order to mitigate the molecular uncertainty between the deposits. 
\section[{a) Geographic Location}]{a) Geographic Location}\par
The study area is located northwest of the Bolivarian Republic of Venezuela, within the Maracaibo Oil Basin, which has an estimated extension of 47,705 km2. To the west-northwest, the basin is bounded by the foothills of the Sierra de Perijá; to the east-northeast by the western foothills of the Serranía de Trujillo; to the southeast by the Andean foothills towards the Motatán River; to the north and imaginary delimited by a line on the border between the states Zulia and Falcón and by the geological line of the Falla de Oca-Ancón. The lines mentioned above are quite arbitrary in the physiographic and geological sense, but they actually correspond to the geo-economic nature of the oil basin as such. At the local level, the study was prepared in Block I belonging to the Lagomar Production Unit of the Maracaibo District, which is located in the north-central part of Lake Maracaibo, occupying an area of 242,324 km2 and being divided into flank East and west flank. Specifically, the study area, called VLA0016 / VLA0033, whose size is approximately 11,888 km2, corresponds to Lagunillas Field and is located in the north-central area of El Pilar in Block I of Lake Maracaibo. Area VLA0016 / VLA0033 structurally limits the west due to a normal type fault with the Urdaneta Lago Production Unit, to the east with the Lama-Icotea Fault, to its north part with an arbitrary limit of the Medium Pink Production Unit and to the south with two faults that are intercepted at the level of the same member Santa Barbara. Table  {\ref 2} shows the UTM coordinates that delimit the study area and Figure  {\ref 1} shows the geographical location of Area VLA0016 / VLA0033. 
\section[{T}]{T}\par
Illustration 1: Geographic Location of the Study Area. Area VLA0033 / VLA0016 in Block I of Lake Maracaibo, Venezuela. 
\section[{b) Methodological Framework}]{b) Methodological Framework}\par
The investigation of this work is descriptive and interpretive. The universe of samples analyzed was 9 wells distributed in areas VLA0016 and VLA0033 of Block I Lagunillas field of the Maracaibo Lake Basin, with emphasis on medium and light crudes from the area (9 Wells), thanks to the fact that they were achieved Perform a greater number of analyzes. It involved the sampling of these wells of the Lagomar Production Unit (U.P. Lagomar).\par
In the first place, we proceeded to search and compile all the information available regarding previous studies and bibliography. The samples were subjected to SARA analysis (separation of the saturated, aromatic, resin and asphalt fractions), to subsequently analyze the aromatic and saturated fractions through gas chromatography coupled to mass spectrometry in order to quantify relative the biomarkers present in the oil, in order to characterize and simulate the deposits. 
\section[{c) Results and Discussion}]{c) Results and Discussion}\par
The results obtained in this investigation, through the processing, analysis and interpretation of the data thrown by the population of crude oils studied, were carried out through a geological study of the area, and its subsequent sampling at the wellhead, which were subsequently analyzed in the laboratory, in order to determine the geochemical characterization of the crudes in the area. 
\section[{d) General Characteristics of Crude}]{d) General Characteristics of Crude}\par
The marine crudes of the Maracaibo Lake Basin, coming from wells completed in different deposits of the geological column of this basin, have been generated mostly by the La Luna Formation.\par
According to the general composition of the crude oils (saturated hydrocarbons, aromatic hydrocarbons and resins+asphaltenes), the percentage of saturated hydrocarbons in relation to API gravity can also provide maturity trends, the higher the saturated content, the lower the aromatic and more asphaltene resins; hence the crudes become lighter crudes like those in this study.\par
Geochemical analyzes carried out on the samples of crude oil from Tertiary deposits included SARA analysis, gas chromatography coupled to mass spectrometry of the Saturated and Aromatic fractions to review the concentration and distribution of biomarkers of these hydrocarbons. 
\section[{II.}]{II.}\par
Relationship of Paraffinity vs. Aromaticity of Thompson (1988)   The characterization, correlation and classification of hydrocarbons is established based on their origin, degree of maturity alteration within the reservoir such as biodegradation, evaporative fractionation water washing, and hydrocarbon mixtures, for this reason the methodology proposed by KF Thompson is proposed ( 1988), which is based on the evidence that the light fraction of some crude oils that contain very high concentrations of aromatic compounds and naphthenes, while the proportion of nalkane compounds is low.\par
Thus, the terms aromaticity are defined (Toluene / n-C7), which is related to evaporative fractionation, and paraffinicity (n-C7-/ Methylcyclohexane), a value that increases with the maturity of the crude In this graph, the direction of the arrows indicates a tendency of increase in the process or that the process is more advanced, for example, in the study area crudes, they are being affected, by an alteration of evaporative fractionation, located in zone A, on the other hand it also shows a good maturity, but as the evaporative fractionation process occurs, residual crudes tend to increase aromaticity, in zone A, while if the light fraction migrated is analyzed, an increase in The paraffinity. According to Halpern (1995)   Looking for the differences in the data of the C7-compounds of unaltered oils compared to biodegraded crude oils of the same family, interaction relationships were constructed in order to emphasize the differences.\par
Parameter Tr1 measures the decrease in toluene which is compound C7; more soluble in water, and therefore it is useful to determine the alteration (water wash). The remaining relationships measure biodegradation and the susceptibility of the compounds involved decreases counterclockwise towards the Tr8 relationship, that is, the more resistant and stable relationship with biodegradation. The Tr6 parameter is composed of compounds that differ significantly in boiling points, so it turns out to be a parameter more resistant (less susceptible) to transformation than the smaller Tr parameters. Consequently, parameter Tr6 is very useful for measuring evaporation caused by inappropriate handling of samples and probably by fractionation-migration effect, in both cases the parameter will increase its value. On the other hand, the star diagram to determine correlations between oils is formed by relationships that are resistant or stable to the transformation processes and that are related to the origin of the crude oils. This means that relationships are virtually invariant within the same family, but that they show significant changes between the crude oils of different families.\par
The C1 to C5 ratios can be used to monitor evaporation or fractionation-migration between samples of the same family. The C1 ratio has a difference in boiling temperatures of -6 between the numerator and the denominator and should decrease with evaporation, while the C5 ratio has a difference of +8 and therefore must increase.\par
The star diagram for the transformation of crudes based on the high percentage of toluene for compound C7, indicates that the crudes under study do not show water wash disturbance, of the nine (9) samples, only VLA1257 wells were differentiated, VLA0121, VLA1570 and VLA0048 for presenting a lower value of toluene in the Tr1 peak, not being affected by this type of alteration. However, it can be inferred that the total of the samples analyzed \hyperref[b5]{(8)} show alterations due to evaporative fractionation. Parameter Tr6 affects all crudes of the analyzed wells, except for well VLA0266, which presents a different alteration process associated more with a fractionation-migration alteration, due to the resistance it opposes with respect to the rest of the crudes.\par
The star diagram to determine correlations of crude oil as stated by Halpern (1988), shows that the samples in studies exhibit a similar profile, coupled with this, it is necessary for parameter C1 in all crude oils except for wells VLA0266 and VLA1570, differ from the others, this being an indication of a possible fractionation -migration, where other authors associate it with a poor handling of the sample during its preparation, additionally the hydrocarbons under study have a high degree of maturation and biodegradation. The results obtained in the analyzes of the composition of the crudes based on their solubility (SARA) and the ternary diagram derived from them, are shown in Figure  {\ref 5}, it is observed that the grouping of data corresponding to all the crudes of the wells studied, they mostly enter the classification of normal crudes, as referenced, The SARA composition for the sands under study, are mainly of paraffinic origin (saturated), and it could be indicated that these crudes because they are at greater depth have a greater maturity level than the raw ones in the shallowest arenas of adjacent areas.\par
Illustration 5: Ternary diagram of the SARA fractions (saturated, aromatic, resins and asphaltenes) with information on the raw materials of the study areaV.\par
Relationship Between pr / n-c17 and F / n-c18\par
In general terms, the relations between isoprenoids are parameters that define the type of contribution of organic matter since a ratio of Pr / Ph less than 1 indicates environments of anoxic deposits and conversely, relations of Pr / Ph greater than 1 indicate environments oxides or disóxicos. If these relationships exceed the value of 3 it is already considered a clear land contribution. When analyzing the data, it is observed that all the samples have a Pr / Ph ratio of less than 1. According to this relationship, an origin of the marine organic matter can be inferred with some contribution of terrestrial organic matter. On the other hand, the relation Pr / nC17 vs. Ph / nC18 according to  {\ref Hunt, (1996)}, also shows values lower than one, which is particular to an organic matter of marine type in conditions of reduction which is attributed to a state of maturity developed, characteristic of the crudes of the area. The bimodal distribution of n-alkanes reveals contribution of marine organic matter, and the Pristano / Fitano ratio indicates conditions of reduction. This is attributed to the advanced state of thermal maturity of the samples. The CPI (Preferential Carbon Index) markers confirm that it is in the presence of a mature oil with possible mixtures, according to Escobar (2007).  
\section[{Thermal Maturity}]{Thermal Maturity}\par
The Ts / Tm ratios are frequently used to determine the degree of maturity. As the degree of maturity increases, Tm increases while Ts remains constant. An increase in the Ts / Tm ratio would indicate an increase in the degree of evolution  {\ref (Philp, 1985)}.\par
If we look at the values of Ts / Tm, they present values of 0.47 and 0.55 respectively. Characterizing the samples as relatively mature. However, Ts and Tm also depend on the type of organic matter, Ts and Tm are biomarkers that are characterized by their resistance to biodegradation.\par
That is why the application of the Ts / Tm ratio as an indicator of maturity should be used wisely, since the oil that has the highest ratios may have suffered some type of biodegradation, while abnormally low relationships may show a provenance. of a carbonaceous mother rock.\par
Crudes from the area of interest under study have a wide range of maturity where the Ts parameters (Ts + Tm) vary between the values of 0.41 to 0.55. In graph 34, it is observed that the relation Ts (Ts + Tm) presents a definite tendency to increase the API gravity of the crudes, the anomalous relationship of maturity Vs API Gravity that the study crudes present, probably the result of some cause of fractionation-migration type Molecular Zoning of Eocene and Miocene Age Deposits, North of Maracaibo Lake Basin alteration as observed in previous results, and these also a good thermal maturity of hydrocarbons as the values grow.\par
Another parameter used to determine the level of maturity is the methylphenanthrene index (MPI-1). This index is based on the distribution of methylphenanthrene and its methylated counterparts. These can be derived from steroids and triterpenoids originally present in the biological starting material; or they may originate from phenanthrene methylation reactions. The isomers that are more stable from the thermodynamic point of view are, 2, 3 methylphenanthrene, versus 1, 9 methylphenanthrene, according to  {\ref Peters et al., (2005)}. They also serve to estimate the percentage of vitrinite reflectance calculated, since it has been observed that they have a linear relationship, according to  {\ref Peters et al., (2005)}. As the following illustration shows, all the samples studied have a vitrinite value of approximately equal 1, which are mature samples and that all of them are within the oil generation window. \begin{figure}[htbp]
\noindent\textbf{}\includegraphics[]{image-2.png}
\caption{\label{fig_0}}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{2}\includegraphics[]{image-3.png}
\caption{\label{fig_1}Illustration 2 :}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{3}\includegraphics[]{image-4.png}
\caption{\label{fig_2}Illustration 3 :}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{6}\includegraphics[]{image-5.png}
\caption{\label{fig_3}Illustration 6 :}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{8}\includegraphics[]{image-6.png}
\caption{\label{fig_4}Illustration 8 :}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{9}\includegraphics[]{image-7.png}
\caption{\label{fig_5}Illustration 9 :}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{12}\includegraphics[]{image-8.png}
\caption{\label{fig_6}Illustration 12 :}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{}\includegraphics[]{image-9.png}
\caption{\label{figure9}}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{}\includegraphics[]{image-10.png}
\caption{\label{figure10}}\end{figure}
 \begin{figure}[htbp]
\noindent\textbf{}\includegraphics[]{image-11.png}
\caption{\label{figure11}}\end{figure}
 			\footnote{© 2019 Global Journals} 			\footnote{© 2019 Global Journals lobal Journal of Researches in Engineering ( ) Volume XIx X Issue VI Version I} 		 		\backmatter  			 \par
Illustration 10: Relationship of the Hópanos with the diagenesis of the crudos in the area of study Integrating the information of the related crudes, it can be observed that the crudes have good maturity induced by the gradual burial of the generating rocks of the Formation La Luna, Gómez and Urdaneta (2013).\par
In this way, a significant amount of light crudes in the Maracaibo Basin have been generated at a relatively late stage of generation. However, it can be seen that biodegradation has also affected some light crudes specifically those of Sands B in the study area. 			 			  				\begin{bibitemlist}{1}
\bibitem[Kaufman et al. (1987)]{b8}\label{b8} 	 		‘A new technique for the analysis of commingled oil and its application to production allocation calculations’.  		 			R L Kaufman 		,  		 			A S Ahmed 		,  		 			W B Hempkins 		.  	 	 		\textit{Proceedings Indonesian Petroleum Association},  				 (Indonesian Petroleum Association)  		1987. October 1987.  	 	 (sixteenth annual convention) 
\bibitem[Nakasone and Miriam ()]{b1}\label{b1} 	 		\textit{Aplicación de la geoquímica orgánica de producción sobre el bloque I, segregación Lagomar},  		 			L Nakasone 		,  		 			O Miriam 		.  		1999.  		 			Lago de Maracaibo. Tesis de grado magister Scientiarum (LUZ). Maracaibo -Venezuela 		 	 
\bibitem[Romero ()]{b2}\label{b2} 	 		\textit{Caracterización Geoquímica de los Yacimientos C-4 VLA-031 y C-5 VLA-031 mediante geoquímica de producción. Bloque I, U.E Lagomar. Tesis-1033},  		 			M Romero 		.  		2007. Venezuela.  	 
\bibitem[Briceño ()]{b7}\label{b7} 	 		‘Comparación e interpretación de dos levantamientos sísmicos 3D, bloque I Lago de Maracaibo Tesis’.  		 			G Briceño 		.  	 	 		\textit{UCV. Caracas}  		1999. p. 99.  	 
\bibitem[Quiroga and Rodrigo ()]{b5}\label{b5} 	 		\textit{Curso Sinóptico de Geoquímica del Petróleo, Revista Técnica de Yacimientos Petrolíferos Fiscales Bolivianos},  		 			A Quiroga 		,  		 			L Rodrigo 		.  		1990. Santa Cruz -Bolivia.  	 
\bibitem[Consultores ()]{b0}\label{b0} 	 		\textit{Estudio Geoquímico de los crudos de las areniscas del Eoceno C y de la Formación La Rosa (Mioceno) de la Cuenca de Maracaibo},  		 			S A Consultores 		,  		 			Csc 		.  		1994. Venezuela.  	 
\bibitem[Bello-Montoya et al. ()]{b12}\label{b12} 	 		\textit{Estudio geoquímico en muestras de aceite y roca de los campos del área Comalcalco-Villahermosa, etapa I},  		 			R Bello-Montoya 		,  		 			E Rosales 		,  		 			V Sánchez-Martín 		,  		 			D F México 		,  		 			Instituto México 		,  		 			Mexicano Del Petróleo 		.  		1986.  	 	 (unpublished report, 70 p) 
\bibitem[Waples ()]{b10}\label{b10} 	 		\textit{Geochemistry in petroleum exploration. International Human Resources Development Corporation},  		 			D Waples 		.  		1985. Boston. p. 232.  	 
\bibitem[Albarède ()]{b4}\label{b4} 	 		\textit{Introduction to geochemical Modeling},  		 			F Albarède 		.  		1995. Cambrige: Cambrige University Press. p. 543.  	 
\bibitem[Krauskopt ()]{b3}\label{b3} 	 		\textit{Introduction to geochemistry. International Student Edition},  		 			K B Krauskopt 		.  		1982. Singapore: McGraw-Hill. p. 617.  	 
\bibitem[Hunt ()]{b11}\label{b11} 	 		\textit{Petroleum Geochemistry and Geology},  		 			J M Hunt 		.  		1995. New York: W.H. Freeman and Company. p. 743.  	 
\bibitem[Talukdar et al. ()]{b6}\label{b6} 	 		‘Petroleum Systems of the Maracaibo Basin’.  		 			S Talukdar 		,  		 			F Marcano 		,  		 			W Dow 		.  	 	 		\textit{¨The Petroleum System-From Source to Trap¨. AAPG Memoir 60; 1st},  				 (Venezuela; Tulsa)  		1994. p. .  	 	 (En: Magoon,) 
\bibitem[Peters and Moldowan ()]{b9}\label{b9} 	 		\textit{The biomarker guide: Interpreting molecular fossil in petroleum and ancient sediments},  		 			K Peters 		,  		 			J Moldowan 		.  		1993. London: Prentice Hall. p. 363.  	 
\end{bibitemlist}
 			 		 	 
\end{document}
